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Analytical Report · 2026

Climate as a Threat to the Economy and Society in the Years and Decades Ahead



Map

Map of risks and impacts

A comprehensive view of how climate change is becoming a global crisis. It is not an isolated environmental problem, but an interconnected system of cascading threats to the global economy, food security, the availability of basic necessities, and society as a whole.

+1.5 °C · ~2028 +2 °C · ~2035–2040 +3 °C · ~2050–2060
Map

Map of the climate crisis

This is not a list of separate risks, but a single self-reinforcing system: impacts occur regularly and across the globe, and are growing in frequency and intensity. They may be interconnected or compound one another's effects. The map reads from top to bottom: the cause triggers a cascade, and each stage places pressure on the next.

01cause

Climate change thresholds


+1.5 °C Extreme events become regular occurrences was expected by ~2035 actually ~2028
+2 °C High risk of severe or catastrophic impacts on societies and economies, including state collapse in vulnerable regions (if current trends continue) expected by ~2050 new data: likely as early as
~2036–2038
+3 °C High risk of extreme impacts, including state collapse worldwide (if current trends continue) expected by the end of the century new data: likely as early as
~2050–2060
Non-linearity. Crossing each threshold does not mean gradual deterioration, but a shift to a different climate regime. Risks grow non-linearly, exponentially increasing pressure on economies, ecosystems, infrastructure and health. The difference between +1.5 °C and +3.0 °C is as critical to civilisation as a rise in body temperature from 38 °C to 41 °C is to a person.


02physics

The planet's response

Natural disasters are becoming more destructive, occurring more often and spreading to new regions previously considered safe. Weather is becoming less predictable. This process is unfolding everywhere, placing pressure on economies and other areas of life. Climate shocks can overlap, significantly compounding damage through their combined effects. All of this is already happening.

Water

Major freshwater sources are gradually deteriorating

Rivers, snow cover, glaciers and groundwater

Heat

More frequent heatwaves and wet-bulb temperatures rising to dangerous levels.

Direct pressure on health and labour productivity.

Drought

Droughts are becoming more frequent, lasting longer and spreading to new regions.

Soil-moisture and hydrological droughts are becoming chronic.

Fires and smoke

Burned areas are expanding, and smoke is travelling over long distances.

Damage to assets is compounded by a hidden impact on health and incomes.

Heavy rainfall and floods

More energy in the atmosphere intensifies extreme precipitation.

Greater strain on urban drainage systems and dams, with a risk of flash flooding.

Storms · hurricanes · hail

Increasing intensity and frequency.

Threat of severe and widespread physical damage.

Sea level

Sea-level rise and coastal flooding.

Flood risk to coastal cities and assets.

Biodiversity and ecosystems

Species loss and ecosystem destruction.

These undermine pollination, fisheries, coastal protection and soil fertility.

Pathogens

Expansion of the range of disease vectors.

Unfamiliar hazards, new costs.

Weather anomalies

Declining predictability. For example, drought can abruptly give way to flooding.

Makes planning and protection more difficult.

Compound risks

Hazards coincide in time and space, or compound one another's impacts.

Heat, drought and fires reinforce one another — a ‘perfect storm’.

Points of no return

Risk of irreversible shifts: AMOC circulation, ice sheets and other climate systems.

The probability is low but increasing. The consequences are catastrophic.
03impacts

Impact on the foundations of life and the economy

Chain reaction. Degradation and disruptions in fundamental systems (fresh water, food, energy and logistics) place growing pressure on the economy and society. In a highly interconnected world, large-scale shocks act as a chain reaction: a failure in one link disrupts other chains, multiplying losses and social consequences worldwide.

Health

Rising mortality and morbidity from heat, wildfire smoke and vapours from volatile compounds. Pressure on healthcare systems and insurance reserves.

Already happening+63% increase in deaths in 2012–2021 compared with the 1990s. The 2022 peak in Europe was ~62,000 deaths. [EEA, ch. 11; WWA, 2025]
Future:

+2 °CEurope: 70% more people than today — around 172 million per year — will face extreme summer heat. In an average year, mortality from extreme heat will rise by around 75%, to ~52,000 deaths per year.

+3 °CEurope: nearly 300 million people per year — more than half the population. Mortality from extreme heat will increase by a factor of roughly 3, to ~96,000 deaths per year.

Water

Freshwater shortages and rising costs for households, agriculture, industry and data centres.

Already happeningOver a 25-year period, 79 major cities imposed large-scale restrictions on water supplies (Barcelona, Los Angeles, Melbourne and Mexico City). [JRC, World Drought Atlas, 2024]
Future:

+2 °C‘Day Zero’ (urban water supplies being cut off) is becoming a recurring risk as early as the 2020–2030s: vulnerable regions include the Mediterranean, southern Africa and parts of North America.

+3 °CThe risk of ‘Day Zero’ becomes chronic and spreads further: India, northern China, North Africa, southern Australia and elsewhere.

Food

Crop losses due to heat, water scarcity and rising water costs → higher prices and shortages.

Already happeningIn 2024, cocoa prices rose by ~300%, coffee by 100% and rice in Japan by 48% — following heatwaves and droughts. [Kotz et al., 2025]
Future:

+2 °CIn key food-producing regions, between 10% and 31% of current production of major crops falls outside its climatic suitability range (South Asia, the Middle East and North Africa, sub-Saharan Africa, South-East Asia, Central America and parts of South America). The range of crops suitable for cultivation narrows across 52% of global cropland. At the same time, the impacts of +2 °C warming could be substantially more severe than the average projection suggests: around a quarter of climate models already project stronger droughts across the world’s key breadbasket regions at +2 °C than the average projection for +4 °C.

+3 °CThe risk increases substantially: between 20% and 48% of current production falls outside its climatic suitability range. In the Middle East and North Africa, South Asia and sub-Saharan Africa, around 60–69% of cropland is at significant risk.

Energy

Risk of nuclear and thermal power plant shutdowns due to high water temperatures, as well as reduced hydropower generation → higher prices and the threat of blackouts. At the same time, demand rises due to cooling needs.

Already happening2026: Hungary: NPP — −50% of national electricity generation; Romania: the entire NPP was shut down — −20% of national electricity generation; Serbia: output of the two largest hydropower plants −70–80%. [BBC; Reuters, 2026]

2022 and 2025: Spain: hydropower −48%; nuclear and thermal power plants in Switzerland and France: temporary shutdowns, wholesale prices tripled. [JRC; WRI].
Actual losses already exceed the projected levels below.
Future:

+2 °CEurope: hydropower plants and water-cooled thermal and nuclear power plants lose up to 10% of capacity. Losses in France — a key energy exporter — could rise to ~20%.

+3 °CEurope: water-cooled thermal and nuclear power plants lose up to 15%–20% of capacity. Hydropower losses increase substantially — in the Mediterranean, they could double or triple.

Supply chains

Falling water levels in major navigable rivers (the Rhine, Danube, Po and Loire) make freight transport more expensive or bring it to a halt.

Already happening2026: Rhine: vessel cargo capacity −67%; petroleum-product freight rates +54% vs the previous record set in 2022; Netherlands: Rhine flow −67% vs the July norm, restrictions on barges, ferry and lock closures. Danube: record-low water levels in Hungary, Serbia and Romania; vessel loads −60–70%, Serbia's fuel imports −75% vs plan. [Reuters; Straits Times; DutchNews, 2026]

2018: Rhine: 132 days of shipping disruption, −0.4% of German GDP. Danube: freight transport in Austria −25% for the year, up to −50% in Q3–Q4 due to low water. [EEA / JRC Atlas; viadonau]

2022: Rhine: barges loaded to 30–40% of capacity, freight rates rose by a factor of more than 5. [DW, 2022]
Future:

+2 °CRhine in summer: average water level −10%, in dry weeks −20%, and in drought years up to −35%. Danube: historically rare low-flow events intensify.

+3 °CRhine in summer: seasonal water level −15–20%, in dry weeks −30–35%, and in extreme periods up to −60%. Danube: extreme low-flow events intensify and water scarcity becomes more frequent.

Industry

Reduced production due to water shortages for industrial processes. Rising raw material costs and product prices.

Already happeningBarcelona, 2024: mandatory 25% cut in industrial water use (textiles). [DW, 2022; EEA]
Future:

+2 °CMandatory water-use restrictions and downtime in water-dependent industries become more frequent in vulnerable regions.

+3 °CThe number of vulnerable regions is growing, while chronic shortages constrain operations and production growth.

Biodiversity

A problem with catastrophic potential. Ecosystems sustain clean water, fertile soils, pollination, food security and protection from extreme weather; businesses depend directly or indirectly on biodiversity [IPBES, 2026IPBES Business and Biodiversity Assessment Summary for Policymakers“Biodiversity and nature's contributions to people underpin the economy, so all businesses depend, directly or indirectly, on biodiversity.”PDF · p. 5; ESOTC, 2025European State of the Climate (ESOTC) 2025“Diverse species and habitats support clean air and water, fertile soils and pollination, contributing to food security, livelihoods and health... regulate the climate and protect against extreme events.”PDF · p. 9].

Future:

+2 °C18% of insects, 16% of plants and 8% of vertebrates may lose more than half of their climatically suitable range. Up to 90% of coral reefs may be lost: they support around 25% of marine life, as well as food or incomes for ~500 million people. [Price et al., 2024 / Warren et al., 2018Biodiversity losses associated with global warming of 1.5 to 4 °C“At 2 °C, these projections of loss fall to 18% of insects, 16% of plants and 8% of vertebrates...”Article · review of the assessment by Warren et al., 2018; IFoA, 2026Planetary Solvency: Tipping into the wild unknown“Coral reefs, which support 25% of marine life, are projected to decline by up to 90% by 2050.”“...the food and economic livelihoods of an estimated 500 million people.”PDF · p. 26].

+3 °C 49% of insects, 44% of plants and 26% of vertebrates may lose more than half of their range. Other ecosystems are also at significant risk: rainforests and mangroves may begin to collapse, disrupting water supplies, food systems, coastal protection and regional weather patterns. [Price et al., 2024 / Warren et al., 2018Biodiversity losses associated with global warming of 1.5 to 4 °C“Climatically driven geographic range losses of more than 50% is projected in ~49% of insects, 44% of plants and 26% of vertebrates for warming of 3.2 °C...”Article · review of the assessment by Warren et al., 2018]; HM Government, 2025Global biodiversity loss, ecosystem collapse and national security (2025)“There is a realistic possibility that some ecosystems... start to collapse from 2030, and others (rainforests and mangroves) start to collapse from 2050.”PDF · p. 2; HM Government, 2025Global biodiversity loss, ecosystem collapse and national security (2025)“If current rates of biodiversity loss continue, every critical ecosystem is on a pathway to collapse... including the collapse of major food sources and fundamental changes to global weather patterns.”PDF · p. 7; ESOTC, 2025European State of the Climate (ESOTC) 2025“Diverse species and habitats support clean air and water, fertile soils and pollination, contributing to food security, livelihoods and health... regulate the climate and protect against extreme events.”PDF · p. 9].


Cascade through supply chains. A local shock propagates through trade links — a drought thousands of kilometres away halts production in an unaffected region. Geographic diversification becomes less effective. At the same time, the world's population is growing (+9% by 2035, +18% by 2050) — demand for resources rises just as the resource base is deteriorating.
04money

Physical risk becomes financial

Property devaluation

Assets in risk zones lose liquidity and value; estimated future losses in the US are up to $1.47 trillion. [FSF, Property Prices in Peril, 2025First Street — Property Prices in Peril: 12th National Risk Assessment (2025)“70,026 neighborhoods (84% of all census tracts) … $1.47 trillion in net property value losses”]

The impact is concentrated in places that continue to attract people and capital.

The limits of the state

A series of disasters could push budgets to their limits.

Relief and recovery compete with debt servicing.

Social division

Access to safety is determined by capital: the wealthy retreat to ‘climate havens’.

Vulnerable groups are trapped in depreciating assets; forced migration increases.

Social unrest

Falling incomes, resource shortages, rising water and food prices, mass climate migration and growing social inequality increase political instability and social tension.

Food price spikes have historically coincided with waves of protests and uprisings.

Conflicts and wars

Political instability and the risks of disputes over resources and armed violence are increasing.

The cascade may include transboundary disputes over water basins, regional conflicts, the growth of extremist groups, organised violence, conflicts between people and the state, civil wars and wars between states. [ IPCC AR6 WGII, Ch. 4IPCC AR6 WGII — Chapter 4: Water"The impact of climate change on shared water resources might increase tensions among states...""Future climatic conditions and population growth are expected to exert additional pressures on managing already stressed basins such as the Nile, the Indus..."ipcc.ch; IPCC AR6 WGII, Ch. 5IPCC AR6 WGII — Chapter 5: Food, Fibre and Other Ecosystem Products"Increasing demands for food, energy and water can lead to domestic and international conflict, including political instability and migration, often in the context of drought.""Rising food prices can affect conflict, political instability and migration..."ipcc.ch; UN-WaterUN-Water — Transboundary Waters"Mismanaged transboundary water supplies have the potential to cause social unrest and spark conflict.""Transboundary waters account for 60 per cent of the world’s freshwater flows. 153 countries have territory within at least one..."unwater.org; World BankWorld Bank — Indus Waters Treaty"The Indus Waters Treaty was signed in 1960 after nine years of negotiations between India and Pakistan with the help of the World Bank...""...it has survived frequent tensions, including conflict..."worldbank.org; Nature Water, 2024Nature Water — Energy trade tempers Nile water conflict"...new electricity trade agreements between Ethiopia, Sudan and Egypt could help resolve the ongoing water dispute over the Grand Ethiopian Renaissance Dam.""The potential impacts... have created political tensions."nature.com; Chatham House, 2021Climate Change Risk Assessment 2021“Armed conflict”“Regional conflicts”“Rise of extremist groups”“Police/military intervention”“Organized crime and violence”“Conflict between people and states”“Civil war and war”PDF · p. 37 ]
05limit

Likely scenarios
(if current trends continue)



Simplification. The diagram is a simplified conceptual model and illustrates only some of the complex interconnections.
Model limitations. The scenarios presented are the results of scientific modelling. Projections may not match actual outcomes, but in climate science the actual impacts often prove worse than projected.
Averages vs extremes. Projections use average figures and the most likely scenarios. Peak years (for example, once every 3–5 years) or less likely scenarios may bring substantially more severe or, conversely, less pronounced impacts.

Part 1

The illusion of awareness

The fact is acknowledged, but neither the market nor science has the full picture. Purpose of the report. Three reasons why the scale of the problem remains unrecognised.

Part 1 · 3 themes

01.1 Established fact

Climate change is an established fact

The scientific consensus is unequivocal. The main causes are the burning of fossil fuels (coal, oil and gas), modern agriculture and other anthropogenic factors.

Transnational corporations, financial institutions, regulators, insurers and consultancy firms recognise the problem. Nevertheless, a comprehensive view of the situation remains rare, and even scientists lack a full understanding of the risks and consequences.


Ignoring climate risks today is no longer an environmental issue but a matter of competence

For an investor, the current situation comes down to five facts:

  1. Climate change is an objective economic factor.
  2. Over the next decade, many asset classes are expected to undergo unprecedented repricing. This process has already begun and will accelerate.
  3. The likelihood of a climate-related financial crisis is high.
  4. There is a window of time before credit spreads and market prices fully reflect these risks.
  5. Investors must independently prepare for these risks and adapt their portfolios—and they must start now.

01.2 Purpose and sources

A unified picture of the changes ahead

The report aims to translate academic knowledge into plain language. We have brought together disparate research to present a comprehensive picture of what our world may become in the near future. The economy and finance represent only one aspect of this transformation.

The conclusions drawn from the data collected require a major reassessment of core development strategies.

The report provides reliable physical benchmarks (the progression towards the +1.5 °C and +2.0 °C thresholds) and describes their cascading impacts. This evidence base makes it possible to grasp the true scale of the changes ahead and begin adapting today.


Moving beyond outdated models

The report draws on more than 200 studies by the world's most respected scientists, macroeconomists, banks and asset management firms.

We draw on the latest data from 2024–2026. These studies fundamentally change the risk picture, but some have yet to be incorporated into the cumbersome mainstream models used by major financial institutions.

The report's reliability is underpinned by four types of sources:

  1. Academic research: studies undergo rigorous peer review by independent scientists before being published in leading scientific journals.
  2. International organisations: official reports by specialised intergovernmental bodies (the UN, WMO, WHO and others).
  3. Institutional analysis: official reports from institutions with unquestioned global authority — central banks, the world's largest insurance and asset management firms, leading rating agencies and other specialised institutions.
  4. News media: in rare cases involving recent events, reports from major global news outlets may be used.

01.3 Three problems

Why the true scale remains unrecognised

Problem 1: systemic complexity and cascading impacts

Climate change affects the vast majority of natural and economic systems simultaneously. The resulting interconnections and cascading effects are so complex that calculating them precisely is inherently difficult, even for the scientific community.

Because of a lack of understanding of these complex mechanisms, the changes under way remain unnoticed by most people. The issue slips from view, and the true scale and severity of the consequences ahead go unrecognised.

Problem 2: even the scientific community still lacks a complete picture of what is happening

No single forecasting model exists that accounts for all aspects and consequences of climate change. Some models project only the physical climate system (ESM), while others project only the economy (IAM). They exchange static data, but do not influence one another in real time and fail to capture feedback loops.

One example of these connections:

At the same time, the mandatory multi-stage review process for new scientific evidence takes years. It takes even longer for these findings to be incorporated into the core macroeconomic models used by governments and companies. The result is an institutional lag: the global market is forced to assess risks using outdated information, creating a vast ‘blind spot’ across the economy.

Problem 3: insufficient action

Climate scientists are quite literally sounding the alarm, but the public remains passive while politicians and corporations continue to profit, worsening the problem.

Far too little funding is allocated to averting catastrophic scenarios. Even less is allocated to adaptation to impacts that are already being felt. At the same time, tail risks (low-probability but catastrophic events) are often underestimated or not considered at all, even in scientific reports, owing to limited resources or insufficient data for modelling.

Part 2

What has already happened

Broken promises and the +1.5°C threshold · climate change’s ‘hidden tax’ on the economy.

Part 2 · 2 themes

02.1 Broken promises · the +1.5°C reality

Broken promises

In 2015, leaders from almost every country in the world agreed to limit global warming to 1.5°C in order to avoid catastrophic consequences. But those commitments were not met. In 2024, the 1.5°C threshold was temporarily exceeded for the first time, and the latest scientific evidence projects that it will be crossed on a sustained basis as early as 2028. [Kirchengast & Pichler, 2025; WMO, 2025]

Consequences of warming to +1.5°C

02.2 Climate tax · the present

Economic impact: the climate tax

In 2024–2025, key institutions whose findings shape economic and financial forecasting—the US National Bureau of Economic Research (NBER), the Potsdam Institute (PIK), a consortium of central banks from around the world (NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system), Bloomberg and the UN—presented fundamentally new estimates of the economic damage caused by climate change.

If global temperature has substantial economic effects, why did they not become apparent after nearly 1°C of global warming since 1960? Because climate change occurs in small increments, its effects are hidden by background economic variability. Because climate change is also permanent, its effects continue to accumulate over time.

NBER · 2025

Key findings on the current situation:

Chapter

Bad news

Emissions continue to rise, warming is accelerating, and the actual impacts at the same levels of warming could be substantially more severe than average projections suggest.

02.3-02.4 · Bad news

02.3 Root cause

Emissions continue to rise

Global greenhouse gas (GHG) emissions are not falling—they continue to rise and set records [Climate State in 2024; UNEP, Emissions Gap Report, 2024]. To illustrate the scale of this contradiction: it is as if, instead of using water to extinguish a burning house, we were throwing coal onto the fire—which is almost literally what is happening.


02.4 Pathway to +2°C and +3°C

Temperatures continue to rise

Decades of ignoring the problem have made it virtually inevitable that, owing to the inertia of the climate system, we will reach the next threshold—2.0°C of warming [Kirchengast & Pichler, 2025; WMO, 2025].

The probability of limiting warming to below 2°C is less than 5% [Rhodium, Climate Outlook, 2025Rhodium — Climate Outlook 2025“the probability of limiting warming below 2°C before the end of the century... remains below 5%”].

The likely period for reaching 2.0°C was identified as 2041–2060 [IPCC AR6, 2023]IPCC AR6 WGI — The Physical Science Basis, SPM (2021). As a result, 2050 became the reference point for many long-term strategies.

Unless urgent action is taken, global temperature will continue to rise, reaching 3.0°C by the end of the century [IPCC AR6, 2023]IPCC AR6 WGI — The Physical Science Basis, SPM (2021).

Investor takeaway

Risk management must now assume a scenario of 2–3°C warming. The bet that ‘everything will sort itself out’, ‘the market will self-correct’ or ‘governments will keep warming at a safe level’ has failed.


Critical divergence from the models

Warming is accelerating

Crucially: the financial world, most international institutions and regulators rely on established estimates that place the +2°C threshold at ~2050 and +3°C at ~2100 (assuming current policies continue), because their calculations are based on conventional, widely accepted climate models. This scenario underpins many assessments of risk and asset values.

However, the latest scientific evidence indicates a sharp acceleration in warming:

Accordingly, in 2025 Germany’s scientific establishment—the societies of physicists (DPG) and meteorologists (DMG)—issued a joint ‘Call for Decisive Action’. The scientists formally report a risk of +3°C being reached as early as 2050, while by 2100 the global temperature increase under current policies could be 4–5°C [ DPG & DMG, 2025 DPG & DMG — Gemeinsamer Klimaaufruf (2025) p. 4: “Bereits bis 2050 besteht das Risiko einer Erwärmung um 3 Grad.” p. 4: “4–5 °C bis 2100 unter den derzeitigen politischen Rahmenbedingungen erwartet.” ].

Also in 2025, NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system (a consortium of central banks from around the world, including the ECB and the Federal Reserve) added a special scenario Current Policies (high climate response). The reason was an acknowledgement that, with the same emissions, climate change could unfold much faster and cause more damage than previously assumed. NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system describes such an outcome as physically plausible (20%) and recommends that regulators take it into account in stress tests. In this scenario, global temperatures reach +2°C in the second half of the 2030s, +2.5°C by 2050 and +3.8°C by 2100. [NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system, 2025NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system — Physical risks in the updated Climate Impact Explorer (2025)p. 6: “we provide data for a physically plausible high-risk future in which the same emissions pathway [...] results in additional 0.9°C.”p. 22: “such an outcome would need to be considered by regulators for physical stress testing purposes.”p. 35, Table 2: high climate response — 2.5°C in 2050 and 3.8°C in 2100.].

‘Prepare for the consequences of faster-than-expected warming’ [Planetary Solvency, 2026Planetary Solvency: Tipping into the wild unknown“Prepare for implications of faster than expected warming”Web].

New reference points

For the rest of the report, dates given in sources, especially ‘2050/2100’, should be read in light of the possibility of revised timelines. At the same time, specific damage estimates may take into account not only temperature increases but also other indicators; for example, estimates of GDP per capita may reflect the corresponding population growth.

Verifying new scientific evidence and integrating it into the regulatory macro models that guide businesses and the public takes years. As a result, the latest evidence on the acceleration of climate change has not yet been incorporated into the main climate and macrofinancial models used by international institutions and regulators. This means that most financial models and risk assessments based on them may underestimate the speed and scale of the threat: [ NGFS, 2025 NGFS — Physical risks in the updated Climate Impact Explorer (2025) p. 23: The baseline Current Policies scenario uses the median climate response. Stronger warming is presented separately as a plausible “what-if” scenario for physical stress testing. ]:

NEW DATA · 2024–2026 +1.5° · 2028 +2° · 2036–2038 +3° · 2050–2060 EARLIER (OFFICIAL) MODELS +1.5° · mid‑2030s +2° · ~2050 +3° · by ~2100 → 2025 2030 2035 2040 2045 2050 2055 2060+ −7 years −14 years −40 years
Diagram 1Warming trajectory: official models versus the latest data. Each threshold is reached 10–40 years earlier than assumed in most financial models. [IPCC AR6, 2023; NASA, 2023; Foster & Rahmstorf, 2025; Kirchengast & Pichler, 2025; Hansen et al., 2025; Zou et al., 2026]

Status of sources The findings confirm that warming has accelerated since 2015: Foster & Rahmstorf detected this with more than 98% confidence, while Zou et al. found it in every satellite and reanalysis dataset examined. Simple projections indicate a risk of reaching +2.0–2.5°C within the next decade (the studies by Foster & Rahmstorf, Hansen et al. and Kirchengast & Pichler were published in peer-reviewed scientific journals; Zou et al. is still undergoing peer review). [ Foster & Rahmstorf, 2026 Foster & Rahmstorf — Global Warming Has Accelerated Significantly (2026) pp. 4–6: After removing the influence of ENSO, volcanoes and solar activity, the acceleration was detected with more than 98% confidence. p. 6: Global temperature began to diverge from its previous trajectory around 2015. ; Zou et al., 2026 Zou et al. — Global warming acceleration in satellite-observed lower-tropospheric temperature (2026) p. 2: Statistically significant trends after 2015 were found in every satellite and reanalysis dataset. p. 7: By 2034, calculations indicate an additional 0.50–1.04°C of lower-tropospheric warming. The +2.0–2.5°C risk estimate is an interpretation of this projection: the authors did not calculate the exact timing or probability of surface-temperature thresholds being crossed. ].

Critical divergence from average scenarios

Impacts could be worse than expected

Average projections conceal a wide range of possible impacts. For droughts across the world’s key breadbasket regions, around a quarter of models project stronger droughts at +2 °C than the average projection for +4 °C. For extreme precipitation and fire weather, the most severe projections at +2 °C exceed the average projections for +3 °C. For fire weather, the highest and lowest estimates at +2 °C differ by more than a factor of four. In other words, higher levels of warming may be reached earlier, while the impacts at those levels could also be substantially more severe [Nature, 2026Bevacqua et al. - Moderate global warming does not rule out extreme global climate outcomes (2026)“For droughts in global key breadbasket regions, precipitation extremes over highly populated areas and fire weather extremes across forests, global climatic impact-drivers at 2 °C of global warming may turn out to be much more extreme than model-averaged projections at 3 °C or 4 °C warming.”“Out of 42 models, 10 models show climate outcomes at a 2 °C warming that are well beyond the multimodel mean at 4 °C of global warming.”“The four worst-case models at a moderate 2 °C warming show an increase in FWI extremes across forests larger than the multimodel mean projection at 3 °C warming...”“...the worst-case model showing an increase more than 4-times larger than the best-case model (+6.5 against +1.5 relative to preindustrial conditions...)”].

Investor takeaway

Even protection that is technically achievable can become impossible when there is no time left to put it in place.


  1. There is far less time for adaptation and preparation. Conversely, risk underestimation, unpreparedness for the consequences and the overall pace at which risks are evolving are far greater.
  2. The broader market has not yet priced in this evidence, creating a temporary window before it is reflected in asset values.

Part 3

World 2.0 — a new risk paradigm

What +2 °C means in physical and economic terms: nonlinear damage, the accumulation effect, the climate tax of the future — and why it is already inevitable.

Part 3 · 4 themes

03.1 Physics of the +2 °C scenario

What does 2 °C mean?

A 2°C rise is not much—unless we are talking about your body temperature or the planet’s. Even a small increase in global temperature causes a nonlinear increase in the frequency and intensity of extreme events. In other words, warming from 1.5°C to 2.0°C will bring more risks than warming from 1.0°C to 1.5°C [IPCC AR6, 2023].

This is a shift to a climate regime similar to that of the early Pliocene, which the planet has not experienced for more than 3 million years [Hansen et al., 2025]. Natural ecosystems, agriculture and infrastructure are not adapted to such conditions. Many organisms cannot adapt to such rapid changes—doing so takes thousands of years of evolution.


Impacts of warming to +2 °C

This is what that world will look like:

03.2 Physical risks → financial risks

Physical risks become financial risks

A 2°C rise poses a direct threat to global economic stability.

At the current level of technological development, there is a high risk of a food and water crisis that will affect every country to some degree [GlaMBIE Team, 2025; IPCC; Heikonen et al., Nature Food, 2025].

The world’s leading financial and scientific institutions warn that insurance markets could collapse in vulnerable parts of the world and that the financial system as a whole could be destabilised [Allianz, 2025Allianz — Rethinking climate adaptation for global resilience (2025)“certain assets effectively uninsurable”; First Street Foundation, 2025First Street — 9th National Risk Assessment: The Insurance Issue (2025)“private insurance companies are effectively labeling areas as uninsurable; property values will deflate”; EEA, 2024].

It is important to consider three amplification mechanisms:

  1. Nonlinear damage: An economy may cope relatively easily with warming from +1.0°C to +1.2°C. But the shift to +2.0 °C could be catastrophic. Why?

    Infrastructure: Dams designed for a ‘100-year flood’ can withstand a modest increase in heavy rainfall. But once a certain threshold is crossed, they are breached, and damage increases not by 10% but severalfold.

    Agriculture: Up to a certain threshold, heat reduces crop yields gradually; once it is exceeded, losses rise disproportionately, rapidly reducing the resulting harvest.

    Labour productivity: Up to a certain threshold, heat merely slows people down. Beyond it, working becomes unsafe: at a wet-bulb temperature of around 31°C, overheating can begin after just 60–90 minutes of moderate exertion [Penn State University ResearchPenn State — Humans can't endure temperatures and humidities as high as previously thought (2022)“actual maximum wet-bulb temperature is lower — about 31°C wet-bulb”; Raymond, C. et al., 2020Raymond et al. — The emergence of heat and humidity too severe for human tolerance (2020)“...a wet-bulb temperature (TW) of 35°C marks our upper physiological limit, and much lower values have serious health and productivity impacts… an upperlimit for survivability under sustained exposure, even with idealizedconditions of perfect health, total inactivity, full shade, absence ofclothing, and unlimited drinking water (9, 10)... severe mortality andmorbidity impacts typically occur at much lower values—for example, regions affected by the deadly 2003 European and 2010 Russian heatwaves experienced TW values no greater than 28°C (fig. S1). In theliterature to date, there have been no observational reports of TW exceeding 35°C and few reports exceeding 33°C (9, 11, 14, 15). ”] Productivity drops not by 5% but severalfold—or, in some sectors, work stops altogether.

  2. The ‘accumulation’ effect and the depletion of resources needed for recovery:

    A single shock: A country can cope with one major flood by drawing on reserves and borrowing.

    A series of shocks: if a megadrought strikes two years later and a hurricane another year after that, the country may lack both the financial and material resources needed for recovery. Each successive shock causes more damage because it strikes an already weakened system. Models from NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system show that damage from a single shock can affect the economy for up to 10 years.

  3. Compound risks: As warming advances, simultaneous disasters in different parts of the world become more likely (for example, drought affecting the three leading grain exporters). The resulting damage does not add up; it multiplies, causing global supply chains to collapse and triggering a food crisis.
Conclusion

As the planet warms, we move ever closer to thresholds beyond which infrastructure, agricultural and economic systems begin not merely to ‘falter’ but to break down.

03.3 Climate tax · forecast for +2 °C and +3 °C

Climate tax: forecast

Looking ahead, the slowdown in growth at warming levels of +2 °C and +3 °C will become even more pronounced:

Losses in potential global GDP per capita.

[NBER, 2025; PIK revised version, 2025; NGFS]

+2 °C−17–20%Equivalent to $32 trillion annually.Losses in potential GDP per capita by 2050 (based on older models; newer data indicate that the +2 °C threshold will be reached not by 2050 but as early as 2035–2040), relative to scenarios in which warming had stopped in 2020 (PIK) and 2024 (NBER), respectively. NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system gives an estimate of −15%, although it accounts for fewer interconnections. In all cases, these figures represent slower growth, not absolute losses relative to 2020–2024 GDP levels.
+3 °C−53%An economy smaller by a factor of 2 than it could otherwise have been.‘Losses in potential GDP per capita by 2100 (based on older models; newer data indicate that the +3 °C threshold will be reached not by 2100 but as early as 2050–2060) amount to 26% for each additional 1 °C of warming. Capital and consumption decline by 51% and 53%, respectively, resulting in a 35% welfare loss in constant-consumption-equivalent terms at 2024 levels. These are losses relative to the baseline pathway of economic activity between 2024 and 2100, not absolute losses relative to the 2024 level (in other words, the economy still grows, but roughly half as fast). The estimates are comparable to the economic losses caused by the Great Depression of 1929, but in this case the losses are permanent’. [NBER, 2025]
Investor takeaway No. 1

Additional losses of tens of per cent of global GDP are no longer an ‘environmental adjustment’, but one of the largest structural factors within the time horizon of current portfolios. Long-term forecasts of growth, equity returns and sovereign debt sustainability that fail to account for this factor are systematically overstated.

Important considerations:

  1. Aggregate figures conceal substantial disparities in damage: a 17% loss in global GDP may mean a 50% loss of GDP for some countries—for example, those in southern regions.
  2. These projections should be treated as a lower bound. This estimate is ‘inherently conservative’ (it understates, or provides a lower bound for, the actual impact). It omits important factors such as the impacts of heatwaves, sea-level rise, tropical cyclones and points of no return, as well as cross-regional ‘spillover’ effects that can significantly amplify the overall impact, and non-market damage such as harm to ecosystems and human health [PIK revised version, 2025].
  3. NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system: the estimate is based on PIK models and excludes extreme disasters (major hurricanes, mega-fires and rare floods of exceptional severity), chain reactions in the financial system (domino effects and financial panic), an insurance-market crisis, supply-chain disruptions, non-market losses (ecosystem degradation, harm to human health and forced migration—all of which are already occurring), the crossing of points of no return, and compound risks—that is, interactions between climate shocks and non-climate shocks (pandemics, other financial crises and wars). At the same time NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system acknowledges that these factors have ‘significant macroeconomic implications’ and pose a risk to financial stability.
Investor takeaway No. 2

The actual losses to the economy could be substantially higher.

03.4 A new landscape for investors

This fundamentally changes the investment landscape

  1. A powerful systemic factor: Evidence shows that the global economy is subject to a persistent, powerful drag. Climate change must be treated as a fundamental macroeconomic factor and monitored as closely as the Federal Reserve’s actions—with the understanding that this ‘regulator’ will never cut rates.
  2. Forecasting errors: Long-term forecasts of GDP and GRP (gross regional product) growth, which underpin financial models, are highly likely to continue being systematically revised downwards. This is because current models are slow to incorporate new scientific evidence, poorly capture—or entirely omit—the accelerating pace of climate change, interconnections and cascading impacts, and often ignore low-probability but catastrophic events (such as points of no return).
  3. Non-diversifiable risk: This newly quantified macroeconomic risk is systemic and difficult to hedge through diversification. It is forcing investors and regulators to reassess the risk premium for entire countries and sectors, which may raise the cost of capital for everyone.
  4. Threat of systemic failure: Today, climate change is seen as slowing growth, but as it intensifies, it poses a real threat of a debt crisis, the collapse of social systems and investment paralysis.

The inevitability of change

The global economy is already locked into a 17% reduction in income (with warming to +2 °C) because of historical carbon emissions and socioeconomic inertia [PIK revised version, 2025].

Investor takeaway

The question is no longer whether there will be a crisis, but how deep it will be and how to prepare for it.

Scientific consensus

This is not a conspiracy theory, but the consensus view held by the overwhelming majority of leading experts. This is not alarmism, but a conservative forecast.

Earth scientists and climate scientists are seriously nervous…

Johan Rockström · Director of the Potsdam Institute for Climate Impact Research (PIK) · source — TED Talks (video)

And, no less importantly for investors, this is a scenario that the world’s largest financial and insurance institutions are already incorporating into their business models (see the Finance section).

Chapter

HEAT, HEALTH AND LABOUR PRODUCTIVITY

Global indicators

Since 1990, almost every risk indicator has worsened. Weather claims lives, reduces people's capacity to work and undermines food security.

Europe

In recent years, Europe has experienced several periods of extreme heat and drought, most notably in 2003, 2007, 2018, 2019, 2022 and 2023. The European temperature record of 48.8 °C was set in Sicily in August 2021; in July 2019, Paris reached 42.6 °C and, in light of the trend, began preparing for possible 50 °C days by mid-century [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)PDF · Ch. 11; Prior, 2023; Cazi & Garric, 2023]. In June 2026, new all-time national temperature records were set: Germany — 41.8 °C, Poland — 40.5 °C, Denmark — 37.0 °C [ZDF / DWD, 2026ZDFheute — Wetter: Diese Hitzerekorde sind 2026 bereits gefallen“Jetzt hat der Deutsche Wetterdienst die technische Qualitätskontrolle der zunächst vorläufigen Rekordmessungen abgeschlossen. In dem Prozess ist nicht nur der Hitzerekord noch einmal nach oben korrigiert worden - auf 41,8 Grad in Möckern-Drewitz in Sachsen-Anhalt.”Web; IMGW, 2026IMGW-PIB — Charakterystyka wybranych elementów klimatu w Polsce w czerwcu 2026 roku“Najwyższą wartość temperatury powietrza (40,5°C) odnotowano 28 czerwca w Słubicach... Jednocześnie jest to najwyższa temperatura powietrza zarejestrowana na stacjach synoptycznych w historii pomiarów w Polsce.”Web; DMI, 2026DMI — Varme og uvejr: Ny dansk varmerekord sat i både Ødum og Odense“Vi har fået en ny varmerekord for den absolut højeste temperatur målt i Danmark. I dag blev der målt 37,0 grader...”Web].

At the same time, Europe remains poorly adapted to extreme heat: in 2022, only about 19% of households had air conditioning, compared with 76% in North America [WRI, 2026World Resources Institute — Europe’s Soaring Heat and the Great Air Conditioning Dilemma“The share of households with air-conditioning units by region in 2022 reveals that Europe (19%) lagged behind other regions, particularly North America (76%)...”Web].

Past · 1981–2010~2 750historical baseline underlying current healthcare systems and insurance models
Now · +1.5 °C~30 000roughly a 10-fold increase; peak years exceed the average — 2022 heatwave: ~62,000 premature deaths
Future · +2 °C~52 000approximately 75% above the current level (+1.5 °C)
Future · +3 °C~96 000roughly 35 times the historical baseline; peak years will be significantly higher
A several-dozen-fold increase in mortality is not a gradual change but a systemic shock to healthcare and social protection; at the same time, it directly reduces labour productivity and consumer activity.
Past · 1981–2010~10 millionlocalised episodes
Now · +1.5 °C~100 million10-fold increase
Future · +2 °C~172 million70% more people than today (+1.5 °C) will experience extreme heat in summer
Future · +3 °C~300 million30 times the historical baseline (more than half of Europe's population)

The risk of extreme events is probably underestimated: extreme heat in Western Europe is increasing faster than climate models projected, so projections may understate the changes [EEA/EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)].

The wet-bulb temperature problem:

Danger arises when high temperatures combine with high humidity. Sweat no longer evaporates properly, and the body loses its principal cooling mechanism. At as little as a wet-bulb temperature of 30–31 °C even a young, healthy person may no longer be able to maintain a stable body temperature. With moderate physical activity, a dangerous rise in core body temperature may begin within 60–90 minutes — at this level, activity can no longer be continued safely. Once the thermoregulatory limit is exceeded, core body temperature may rise by approximately 0.74–0.93 °C per hour even with minimal activity or light walking.

Shade, water and rest reduce the strain but do not eliminate the problem: if the body can no longer dissipate heat on its own, active cooling, such as air conditioning, is required. Otherwise, body temperature will continue to rise and the person may develop heatstroke — a condition that requires emergency treatment and can be fatal. The risk is higher for older people, children and people with chronic illnesses, and the dangerous threshold may be lower; as their condition worsens, people may no longer be able to assess it accurately because of weakness, dizziness or confusion. [Penn State, 2022Penn State (2022)“the actual maximum wet-bulb temperature is lower — about 31°C wet-bulb…”“critical wet-bulb temperatures ranged … from 30°C to 31°C…”“even for young, healthy subjects”“a person’s sweat will not evaporate at that skin temperature.”“they could no longer adequately regulate their body temperature…”“Older people, people on medications, and other vulnerable populations will likely have a tolerance limit below that.”; Georgia Tech Urban Climate LabGeorgia Tech Urban Climate Lab“a wet bulb temperature of 87°F … is found to induce a fever within 60-90 minutes of exposure at a moderate activity level”“the 87°F threshold at which outdoor activities cannot be safely continued.”“outdoor activities such as landscaping, construction, municipal services … and athletic events would pose an acute health risk and should be discontinued.”; Cottle et al., 2022Cottle et al., 2022 (Journal of Applied Physiology)“uncompensable … heat stress … WH: MinAct, 0.74, LightAmb, 0.87; HD: MinAct, 0.71, LightAmb, 0.93°C/h”“can be used to estimate the time to reach a target core temperature…”; CDC, 2026CDC, NIOSH — Heat-related Illnesses“Heat stroke is the most serious heat-related illness.”“body temperature can rise to 106°F or higher within 10 to 15 minutes.”“Heat stroke can cause permanent disability or death…”“Symptoms of heat stroke include: Confusion, altered mental status, slurred speech”“Loss of consciousness”; CDC, 2024CDC — Heat and Health“People aged 65 years or older are at higher risk for heat-related illness.”“Infants and children are more sensitive to heat…”“People with chronic medical conditions are more likely to have a serious health problem during a heat wave…”]

MapImpact of climate change under a global warming scenario of +2 °C. From left to right: additional economic costs (% of GDP), population exposure to risk (% of population), mortality from non-optimal temperatures. [EC, JRCNinth Report on economic, social and territorial cohesionMap 4.1 The impact of climate change under a 2°C global warming scenario in NUTS 3 regions, 2050PDF · p. 165]
Map 4.1 The impact of climate change under a 2°C global warming scenario in NUTS 3 regions, 2050

Loss of labour and income: world and Europe

Heat reduces working hours and labour productivity, especially in sectors involving outdoor work. Adaptation measures are critical to worker safety and productivity [van Daalen et al., 2022; EEA, 2022].

In 2024, heat stress caused a record 640 billion potential working hours to be lost (+98% compared with the 1990s), pushing global income losses above $1 trillion for the first time. The agricultural sector bore the brunt, accounting for 63.5% of the time lost [Lancet Countdown, 2025The 2025 report of the Lancet Countdown on health and climate change“globally, 640 billion potential work hours were lost due to heat exposure in 2024... a record-high global potential loss of income worth $1·09 trillion.”PDF · p. 12].

At +3 °C of global warming, labour productivity is expected to fall by 33% in Africa's outdoor sectors and by 25% in Asia. By 2060, indirect effects transmitted through global supply chains will account for 12% to 43% of global economic losses from heat [10NICS, 202510 New Insights in Climate Science 2024/2025“3°C of warming would cut labour effectiveness by 33% in Africa's outdoor, high-exposure sectors and 25% in Asia's... indirect effects on global trade and supply chains are projected to account for 12–43%.”PDF · p. 32].

Air pollution

The combination of wildfire smoke and volatile substances evaporating from scorching asphalt in hot weather worsens air quality.

In Europe, air pollution is the ‘leading environmental health risk’: in 2020 alone, it caused 253,000 premature deaths. Almost 96% of the urban population breathes air that does not meet the latest WHO guidelines [JRC].

  • Geography of risk: the greatest damage to health (years of life lost) is concentrated in Bulgaria, Croatia, Poland, Slovakia, Hungary and Romania.
  • Link to poverty: pollution levels in the poorest EU regions are consistently one-third higher than in the wealthiest, and the gap is not narrowing. The main reason is ‘energy poverty’, which forces people to use low-quality coal and even waste for heating.

Health and biological risks

Infectious diseases

Dengue fever — an acute viral disease that is transmitted to humans through the bites of infected mosquitoes and can be fatal. It was previously confined to the tropics and subtropics.

Warming is expanding the range of disease vectors: around half of the world's population is now at risk of dengue fever. The largest global outbreak on record occurred in 2024, with 14.2 million cases. [10NICS, 202510 New Insights in Climate Science 2024/2025“Dengue fever surged over the past two years to 14.2 million reported cases in 2024, the largest global outbreak ever recorded... About half of the world's population is now at risk of dengue.”PDF · p. 29].

Climate suitability for transmission of the virus by the mosquito Aedes albopictus has increased by 48.5% compared with the 1950s [Lancet Countdown, 2025The 2025 report of the Lancet Countdown on health and climate change“The estimated global average R0 for Ae albopictus and Ae aegypti mosquitoes increased 48·5% and 11·6%.”PDF · p. 16]. Climate change caused up to 40% of new dengue cases in several countries in the Americas [10NICS, 202510 New Insights in Climate Science 2024/2025“A recent study suggested climate change was responsible for up to 40% of dengue cases in some countries in the Americas.”PDF · p. 30].

Investor takeaway

Mortality figures are the end point, reflecting the far broader impact of heat on health, particularly for children and older people. Labour productivity is hit hardest in outdoor work (agriculture, construction, street trading and public utilities), as well as in regions where air-conditioning coverage is low — as it is in Europe, for example.

Healthcare costs, recurring cooling costs and infrastructure wear will rise.

Chapter

Water and droughts


04.2 Water and drought

Where water comes from — and why the entire system is deteriorating

A single diagram is enough to understand the risks to rivers, glaciers and groundwater. Fresh water comes from two main sources: surface water (rivers and lakes) and groundwater.

Water bankruptcy diagram: sources of water inflows, how water is used, and the point at which water use exceeds inflows.
Diagram 2‘Water bankruptcy’: when water use exceeds inflows, society begins consuming its natural capital — aquifers, glaciers, soil moisture and surface water. [UNU-INWEH, 2026UNU-INWEH — Global Water Bankruptcy: Living Beyond Our Hydrological Means in the Post-Crisis Era“Water Assets = Checking account + Savings account”“Insolvency = Water Income < Water Expenses”“Irreversibility = Irreparable Natural Capital Damages”]

Rivers and lakes are replenished in three ways:

  1. Direct precipitation.
  2. Melting snow and glaciers. Glaciers act as strategic ‘water towers’: they store winter precipitation and release it in summer, maintaining stable river flows during the driest period.
  3. Slow seepage from groundwater.

Groundwater (subsurface water) is replenished in two ways:

  1. The bulk consists of ‘fossil’ reserves accumulated over hundreds and thousands of years.
  2. It is also recharged by precipitation.

Cities usually draw on all these sources at the same time, where available.

Climate change strikes every component at once

  1. Sources are drying up: precipitation is declining; glaciers and snow cover are disappearing (many regions are projected to lose their glaciers completely within the next few decades).
  2. Surface water is drying up: rivers and lakes are becoming shallower as their sources of replenishment decline and evaporation increases with rising temperatures.
  3. The strategic reserve is being depleted: excessive groundwater extraction is increasing; in coastal areas, this also leads to irreversible salinisation of groundwater by seawater [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)].

Around 75% of the world's population lives in 101 countries that are losing fresh water. Satellites are recording an unprecedented loss in the total mass of continental fresh water (including groundwater, soil moisture, snow and surface water). The world's dry regions are drying faster than wet regions are becoming wetter, and the area of arid land is expanding rapidly [«Unprecedented continental drying…», Science Advances, 2025].

Europe

For the first time ever, the European Commission has called on Member States to cut water consumption by 10% by 2030 — a direct signal of systemic water scarcity [European Commission, 2025European Commission — European Water Resilience Strategy, 3 June 2025It sets an objective to improve water efficiency in the EU by at least 10% until 2030 and recommends Member States to set their own targets…eea.europa.eu].

Pressure on water resources will intensify, with Southern Europe facing severe water stress. Water scarcity is increasing competition between economic sectors... Europe's water management is poorly adapted to these rapid changes, threatening long-term sustainability... Europe will face more frequent droughts, floods and sea-level rise, as well as complex climate risks. Prolonged droughts will become more frequent, exacerbating water stress and harming society, the economy and ecosystems [EEA, 2025EEA Thematic Briefing“Pressure on water resources will increase, with southern Europe facing severe water stress. Insufficient water resources intensify competition across economic sectors... Europe’s water management is poorly-adapted to this rapid change, compromising longer-term resilience... Europe will face more frequent droughts, floods and rising sea levels, as well as compound climatic risks. Prolonged droughts will become more common, worsening water stress and impacting society, the economy and ecosystems.”eea.europa.eu].

Summer water scarcity conditions across Europe, 2022
MapFigure 1. Summer water scarcity conditions across Europe, measured by the water exploitation index plus (WEI+) for sub-river basins, 2022 [EEA, 2025EEA Thematic BriefingWater and climate impactseea.europa.eu]
Investor takeaway

This is not simply a decline in water availability — it is the breakdown of the entire hydrological system. The world faces a growing threat of catastrophic disruption to water resources, undermining the prospect of a sustainable future for all.


04.2.1 The baseline and the shift in the drought regime

The hydrological ‘normal’ is ceasing to exist

In 2024, an area covering 60% of the world's river catchments deviated from normal — it was either too dry or carried too much water. Over the past six years, only one-third of river flows were classified as ‘normal’. The data indicate persistent disruption to the volume and distribution of surface fresh water [WMO, State of Global Water Resources, 2024–2025].

Investor takeaway

The hydrological ‘normal’ is ceasing to exist as a reference point: only one-third of the territory behaves ‘as before’, while two-thirds show anomalies. Risk models, insurance pricing, infrastructure design and agribusiness based on the ‘normal’ of past years all systematically underestimate risk.


04.2.2 Source 1 · rivers: falling water levels

Rivers: the economy's key arteries are drying up

European water security has been undermined at every level: the amount of available water is declining, its quality is deteriorating and demand continues to grow [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)]. The first source — rivers — is already drying up.

Water stress in Europe: population and river flows

[EEA, EUCRA, Ch. 5, p. 129; JRC]

Now · +1.5 °C85 millionpeople in Southern Europe live where annual water consumption is close to the limit of renewable resources — the safety margin may be insufficient for a prolonged drought. At peak demand, Spain, Greece and Portugal consume 40–80% of their renewable water, while Cyprus consumes more than 100%
Future · +2 °C94 millionunder water stress in Southern Europe — the severity and frequency of shortages will increase; river flow on low-flow days will decline by up to 40% in the far south of Spain, as well as in Portugal, Greece and France
Future · +3 °C104 → 295 million104 million under water stress in the south; a 40% decline in river flow extends across most of Southern, Western and Central Europe, including Italy; the shortfall expands across the entire EU — 295 million people
A 40% decline in river flow amounts to the collapse of the river system: a critical threat to hydropower and nuclear power, industry, agriculture and river transport.
Case study: South America — a preview of the future One country in one year: Amazonian rivers at their lowest in 120 years — and, at the same time, the worst flooding in southern Brazil in 80 years. The economy is torn apart by shocks moving in opposite directions. Expand

The situation in the Amazon and the La Plata basin is a warning to the entire world [WMO, State of Global Water, 2025].

  • The Rio Negro at Manaus fell to its lowest level in 120 years (12.11 m); the Madeira River reached a 60-year low.
  • At the same time, southern Brazil experienced its most destructive flooding in 80 years, causing damage and breaching dams.
Investor takeaway

A single country faced both historic lows in its rivers (halting grain and ore logistics) and historic highs in flooding (destroying infrastructure). The economy is torn apart by shocks moving in opposite directions: some regions are paralysed by low water, while others are flooded.


04.2.2.1 Logistics chains

Rhine — the conveyor belt of EU industry

The Rhine is the main water artery of Europe’s industrial core. It connects Switzerland, France, Germany, the Netherlands, Belgium and Liechtenstein to the North Sea and the Port of Rotterdam, which handles a substantial share of Europe’s imports and exports. In particular, around 80% of Germany’s domestic inland water freight traffic moves on the Rhine. [Destatis, 2022German Federal Statistical Office — Inland waterways transport“Most of that freight (86.3%, or 71.1 million tonnes) was carried completely or partly on Germany’s most important inland waterway, the river Rhine.”Web] Low water on the Rhine therefore affects logistics, energy and industry across several countries.

Problem: shrinking Alpine snow and glaciers reduce the Rhine’s summer flow. At the same time, rising air temperatures increase evaporation, while earlier snowmelt reduces the amount of water available for summer. [Deltares, 2026Deltares — 17 questions about drought and low water levels in the Rhine and Meuse“A relatively warm spring: the non-permanent snow melted earlier than usual. Evaporation was also higher than in other years.”Web]

Already happening +1.5 °C

2018 — a record low water level was set. Navigation on the Rhine was disrupted for 132 days. Companies in the chemical, steel, paper, metals, construction materials, agriculture and petroleum-products sectors were affected. This event alone cost Germany 0.4% of GDP. [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024) / JRC Atlas]

However, 132 days of disrupted navigation did not mean 132 days of a complete shutdown. In 2018, the most severe phase of the shutdown lasted around 20 days. Modelling shows that even today, in worst-case scenarios, a shutdown could last up to 130 days, while periods of reduced vessel loading could reach 200 days per year [Campoverde et al., 2025]. Vessels are also in short supply: “we are fully booked,” carriers report [DW, 2022].

BASF case (Ludwigshafen)

Around 40% of supplies to the world’s largest chemical company normally move along the Rhine. Before the 2018 crisis, 5–10 cargo vessels supplied the site every day. When water levels fell, BASF was able to replace only around one-third of the lost shipping capacity with pipelines, trucks and rail. Fully replacing barges would require an additional 1,600 trucks a day — not a viable option [DW, 2022].

2022 — the 2018 record was broken. Barges could carry only 30–40% of their normal loads, while freight rates rose more than fivefold, again hitting Germany’s GDP. Other major rivers, including the Po and Loire, also fell to very low levels. [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024) / JRC Atlas]

2026 — the 2022 record was broken. In July, Rhine flow was about 67% below normal. In many locations, vessels could carry only 20–30% of their normal loads, while at one of the largest inland ports they could carry around one-third. Rates for transporting petroleum products exceeded the previous 2022 record by 54%. In the Netherlands, ferry routes, some locks and harbours were closed. [Reuters, 2026Reuters — Low water hampers Rhine river shipping in Germany, transport costs rise“Vessels are often able to sail only 20% full, with loads having to be divided among several ships.”Web · 13 July 2026 / Straits Times, 2026The Straits Times — Low water on Germany’s Rhine river threatens new blow to economy“vessel loading capacities have dropped to about one-third of their usual levels.”“prices hitting €200 ... previous record of €130 a tonne set in August 2022”Web · 6 August 2026 / DutchNews, 2026DutchNews — Dutch houseboat owners left high and dry by falling river levels“The Rhine sank to its lowest recorded level ... while the flow in the river is one-third of its normal level for July...”Web · 6 August 2026 / DutchNews, 2026DutchNews — Ferries cancelled as rivers drop to record low levels in drought“Restrictions have also been imposed on river barges ... sluice gates have been closed or limited to a few openings a day...”Web · 3 August 2026]

Major rivers — vital transport arteries and sources of freshwater — are becoming systemically vulnerable.

Projected summer water levels in the Rhine

The successive record lows of 2018, 2022 and 2026 call existing projections of future Rhine water levels into question.

Decline in water level relative to the baseline

[Deltares, 2023; ICPR, 2024; Campoverde et al., 2025]

+2 °C−10% / −20%seasonal average −10% (up to −17% in ‘bad’ years). In the driest weeks −20% (up to −35%). Vessels are forced to travel half-empty. Transport costs and delivery times increase
+3 °C−15–20% / −30–35%seasonal average −15–20% (up to −48% in ‘bad’ years). In dry weeks −30–35% (up to −60%). With a 30% decline, even costly dredging does not help. Navigation comes to a complete halt for standard vessels
The Rhine is a conveyor belt for EU industry. At +2 °C it becomes substantially more expensive, slower and less reliable. At +3 °C it could stop.

04.2.3 Source 2 · glaciers and snow

Glaciers and snow: irreversible collapse of Europe's ‘water towers’

Natural freshwater reservoirs that feed rivers in summer are disappearing at a record pace — faster than previously expected — and their loss is irreversible over investment horizons. For the third consecutive year, all 19 glacier regions worldwide are losing mass; for most regions, the point of no return — ‘peak water’ — has already been passed [WMO, State of Global Water Resources, 2024].

Glacier mass loss: world / Alps

[Zekollari et al., Science, 2025]

Already locked in · inertia−50% / −70%even if warming stopped today: the world would lose around half of its glacier mass, and the Alps around 70% of their ice. This is a key source of summer water for the Rhine, Rhône and Po — and thus for the economies of Germany, France and Italy
+2 °C>−60% / −80%global losses exceed 60%, while the Alps lose around 80%: a fundamental structural shock to the EU's industrial heartland
+3 °C−77% / <5%loss of 77% of global glacier mass; less than 5% of the ice remains in the Alps — effectively a complete disappearance within this century
Central Europe is the region responding fastest: 80% of the losses will occur in less than 50 years.
Investor takeaway

In the coming decades, the key source of summer water for the Rhine, Rhône, Po and Danube will effectively cease to exist. This means a structural decline in summer river levels, threatening urban water supplies, production, shipping, nuclear-plant cooling, hydropower generation and agriculture in the EU's industrial heartland.


04.2.4 Source 3 · groundwater: depletion

Groundwater: a non-renewable reserve is being consumed at an accelerating rate

More than one-third of the planet's aquifers are being depleted rapidly [Richey et al., Water Resources Research]. Groundwater depletion accounts for 68% of the total loss of fresh water from non-glaciated continental regions [«Unprecedented continental drying…», Science Advances, 2025]. Groundwater is already being depleted by excessive pumping, especially in Southern Europe. In future, this shortage will spread across almost all of Europe [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024); JRC].

Groundwater reserves take decades or centuries to replenish — their loss is effectively irreversible within an investment horizon. Dependence is enormous: half of the world's population obtains its drinking water from groundwater, which also supports around 40% of irrigated agriculture [UN World Water Development Report, 2022].

As groundwater is depleted, its level falls. Most wells in a given region are drilled to roughly the same depth — down to the first aquifer — so hundreds or thousands of wells may stop working almost simultaneously as the level falls [World Drought Atlas, 2024]. Drilling deeper is difficult, expensive and slow: costs and energy requirements rise exponentially, and every additional metre makes the task harder.

Direct measurements of the largest aquifers

36%aquifers — sustained decline in levels (an average of −0.2 m/year)[Nature, 2024]
30%aquifers — the decline accelerated sharply in 2000–2022 compared with 1980–2000[Nature, 2024]
12%— a ‘rapid’ decline of more than 0.5 m/year: immediate risks to infrastructure and agriculture[Nature, 2024]
x4the rate of depletion exceeds the rate of recharge where recharge occurs[Nature, 2024]

Excessive pumping is not the only problem: more than 80% of aquifers where the decline is accelerating have also experienced less precipitation over the past 40 years. The ‘hotspots’ of decline are precisely the regions critical to global food security: Spain (the Guadiana basin), the United States (California's Central Valley and the southern Great Plains), Iran, the North China Plain and the Indus Basin [«Rapid groundwater decline and some cases of recovery in aquifers globally», Nature, 2024].

Investor takeaway

The depletion of strategic freshwater reserves is a large-scale (affecting more than one-third of all aquifers) and accelerating (deteriorating rapidly in one case in ten) global process. It is occurring in the world's most important agricultural regions, creating a direct threat to global food security and associated financial risks.

Another problem: no one knows exactly how much water remains

No one knows exactly how much water remains in groundwater aquifers, and this ‘severely limits the ability to assess the sustainability’ of their use. ‘The volume of usable global groundwater reserves is largely unknown’; ‘in most cases, we do not know how much groundwater is held in storage’ [Uncertainty in global groundwater storage estimates in a Total Groundwater Stress framework, 2015; Reinecke et al., 2023].

Investor takeaway

It is as if you did not know how much money was in your wallet but were forced to spend it.


04.2.5 Salinisation · warming · demand · conclusions

Scarcer, warmer, dirtier — and increasingly in demand

Salinisation: irreversible loss of fresh water and land

Sea-level rise and groundwater depletion lead to saltwater intrusion in coastal regions. This process makes drinking-water sources unusable without costly, energy-intensive desalination.[EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)].

Warming and pollution

Some of the remaining water is becoming warmer and dirtier. Heavier downpours and floods wash fertilisers, wastewater and other substances off fields, increasing the cost of water treatment. This also triggers toxic algal blooms (eutrophication), creating risks to public health (toxins), tourism (unsafe bathing), fisheries (fish kills), industry and agriculture.

Rising demand against falling supply

In Southern Europe, water withdrawals for cities have risen by 20% over recent decades, and withdrawals for agriculture by 8%. Continued warming and development will drive further increases, creating direct competition for an increasingly scarce resource [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)].

Structure of water use and risks to the largest users

[EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024); JRC Atlas]

Energy · 37%risk of nuclear, thermal and hydroelectric power plants shutting down because cooling water becomes scarce or too warm (32%), or because there is too little water for generation
Agriculture · 28%(46% according to the JRCEuropean Commission's Joint Research Centre Atlas) — crop losses due to a direct shortage of water for irrigation
Population · 20%threats to health and rising utility costs due to drinking-water shortages and poor water quality
Industry · 13%reduced production due to insufficient water for industrial processes; plus river transport — logistics come to a halt as waterways become shallower
This is not simply water scarcity but the systemic degradation of Europe's entire water resource base: scarcity is turning from a regional problem in the south into a systemic risk to the entire EU economy.
Final conclusion on water

The problem is global and unprecedented — a systemic shift in the global water cycle. Because its main drivers are the depletion of groundwater and glaciers, which take centuries to recover, this represents an irreversible loss of natural capital.

For Europe, there is less fresh water, and what remains is dirtier and warmer. The era of ‘cheap water’ is ending; there will be less water with every passing year — not ‘in 1,000 years’, but now.


04.2.6 Another consequence · land subsidence

Land subsidence: a silent risk to real estate and infrastructure

Land subsidence, caused primarily by groundwater extraction, is a large-scale and underappreciated risk to cities. In 28 of the largest US cities, at least 20% of the land is sinking, affecting ~34 million people; the process poses a direct threat of structural damage to tens of thousands of buildings and critically exacerbates flood risks [«Land subsidence risk to infrastructure in US metropolises», Nature Cities, 2025].

>10%of the land in New York, Chicago, Houston and Dallas is sinking at more than 3 mm per year[Nature Cities, 2025]
29 000buildings are located in areas at high and very high risk of damage[Nature Cities, 2025]
80%of subsidence is linked to groundwater withdrawals[Nature Cities, 2025]

This is a silent, ‘latent’ risk: infrastructure may be imperceptibly compromised over many years, while the damage becomes apparent only once it is already serious or catastrophic. These are hidden liabilities accumulating on asset owners' balance sheets.

Investor takeaway

Beyond the direct risk of flooding, real-estate and infrastructure investors must account for the risk of structural damage from land subsidence. Water risk has two faces: groundwater depletion creates both a risk of resource scarcity and a risk of physical destruction of assets at the surface; the two must be assessed together. For coastal megacities such as New York and Houston, this is a double blow: the land is sinking to meet the rising sea.


04.2.7 ‘Day Zero’ case studies

‘Day Zero’: when a city runs out of water

‘Day Zero’ — the term for the day on which the authorities shut off the water supply because of a shortage. In recent years, Cape Town (South Africa, 2018), Chennai (India, 2019), São Paulo (Brazil, 2015), Barcelona (Spain, 2021–2024) and Tehran (Iran, 2025–2026) have faced this reality.

  • Around 25% of the world's cities already face persistent water stress and scarcity. Over the past 25 years, drought has forced 79 megacities to impose large-scale water restrictions, including Los Angeles, Melbourne and Mexico City [JRC, World Drought Atlas, 2024JRC, World Drought Atlas, 2024].
  • The 100 cities where water risks will increase most by 2050 are home to 350 million people; almost half are in China, while other hotspots include South Asia, the Middle East, South America and Africa [WWF, 2020].

‘Day Zero’ is becoming a recurring risk in some regions as early as the 2020s and 2030s. Even quadrupling the length of time for which reservoirs can sustain water supplies during a drought helps in only 8% of cases [Ravinandrasana & Franzke, 2025Nature Communications — The first emergence of unprecedented global water scarcity in the Anthropocene (2025)"An increase in TRD, quadrupling the TRD, will affect the ToFE of the 8% of the DZD-prone regions, causing later emergence..."PDF · p. 4]

Case study 1: Barcelona (2021–2024) — technology at its limits An unprecedented drought for the region: a precipitation deficit of more than 50% against the baseline for three consecutive years. Desalination and water reuse postponed ‘Day Zero’ but did not avert it: without strict conservation, it would have arrived in early 2024. Expand

Catalonia experienced an unprecedented drought: precipitation was more than 50% below the baseline for three consecutive years. This was not ‘another drought’ — there had been nothing like it in the entire 100-year observational record. The reservoirs supplying an urban area of 6 million people were emptying rapidly.

Action 1 — technology at its limits. The city brings every reserve into service: one of Europe's largest desalination plants and a wastewater-reuse system. The unit cost of water increases by more than a factor of 2. But this is not enough — reservoir levels continue to fall.

Action 2 — unavoidable restrictions. The government declares a state of emergency. Increasingly stringent restrictions are imposed, directly constraining the economy:

  • agriculture: compulsory reduction in water use by 80%;
  • industry: reduction by 25%;
  • residents: reduction by 20% (a daily per-person limit is imposed).

Action 3 — conflicts over water. Conflicts arise within Spain (Catalonia versus Aragon) and internationally: Spain reduces flows in shared rivers, leaving Portugal with one-third less water than it is entitled to under international agreements.

Temporary relief: spring 2024 was the first season with normal precipitation in 3.5 years.

The analysis reveals a dangerous threshold:

  • even with all desalination and wastewater-treatment plants operating, ‘Day Zero’ would still have arrived in early 2024 without strict conservation by residents;
  • without desalination plants and water reuse, the reservoirs would have dried up completely as early as summer 2023.

What desalination requires

  • Access to salt water (not available to everyone).
  • Investment of ~€700 million in 3 desalination plants.
  • Around 400 GWh of electricity a year just to operate these plants (comparable to the output of a nuclear power unit).
  • Acceptance that these measures will cover only ~25% of demand.
  • A 4–5-year wait for capacity to come online, with the region remaining at risk throughout.
  • A way to address a severalfold increase in the unit cost of water.

Conclusions: (1) desalination is available only to those with access to salt water; (2) it replaces dependence on free water with dependence on expensive electricity — a classic cascading risk; (3) the energy system is itself a victim of climate change (see topic 04.8, ‘Energy’): 90% of Catalonia's grid is overloaded, and connecting desalination plants requires a multibillion-euro upgrade.

Economic consequences (2022–2024)

−18%GDP of Catalonia's agricultural sector
−21/35/40/58%decline in yields: wine / cereals / wheat / olive oil
up to −25%losses to industrial production (textiles, for example) due to compulsory restrictions
12% of GDPtourism: hotels were forced to incur multimillion-euro costs for their own desalination systems

‘Climate whiplash’ (October 2024): a multiyear drought was followed by catastrophic flooding in the neighbouring region of Valencia. The dry, compacted soil could not absorb the torrential rain, multiplying the severity of the flood (a compound event). The Valencian government had to request €31.4 billion in emergency aid; the preliminary estimate of economic losses was €17.5 billion [WMO, State of Global Water, 2025].

Status in 2025: the drought is not over, some restrictions remain in place, and reservoirs in southern Catalonia are virtually empty. The region's economic and demographic development is now directly constrained by water scarcity.

The Catalonia case is not a local problem but a demonstration of Europe's new economic reality: climate shocks are already directly constraining economic activity, requiring massive, unavoidable investment and creating cascading energy, political and social risks. Drought was once a shock that could be waited out; water scarcity is now becoming a chronic condition. Even with new technology, financing and time for adaptation, the system remains vulnerable — the next drought could return it to the brink of collapse. This is happening at +1.5 °C; at +2 °C and +3 °C the situation will be substantially more severe and widespread.

Case study 2: England and Scotland — a water crisis in a ‘rainy’ country In the East of England, a ban on expanding water supplies for businesses is in force until 2033; the largest operator, Thames Water, is on the brink of bankruptcy with £16.8 billion in debt; by 2055, England will face a water shortfall of 5 billion litres a day. Expand

At the current level of warming, it is not only southern regions that are under threat. The United Kingdom — a country with a rainy climate — is facing a systemic water crisis. In 2022, the officially recorded temperature exceeded 40 °C for the first time in history, while more than one-quarter of river flows were classified as exceptionally low.

1. A direct ban on economic growth

In key agricultural and industrial regions of the East of England, a long-term ban (until 2033) has been imposed on expanding access to water supplies for businesses. For water-intensive sectors — agribusiness, data centres and beverage production — development in these regions is becoming almost impossible or extremely difficult [Alpheus, 2025; BBC, 2024]. The consequence: a ‘risk of strangling UK economic growth’ [Alpheus, 2025].

2. Cascading crisis: timeline

Trigger: the 2022 drought — the worst in 40 years; spring 2025 — the driest in 130 years; the temperature reached 40 °C for the first time [Thames Water, 2023; Guardian, 2025].

  1. Demand rises: extreme heat causes water demand to rise by 40%.
  2. Supply falls: water levels in rivers and reservoirs fall sharply. London came dangerously close to running out of water. In 2022, water-use restrictions affected up to 15 million people; in 2025, the crisis was deeper and bans had to be introduced much earlier [Guardian, 2025].
  3. Reserves fail: a key desalination plant was unavailable because of maintenance scheduled on the basis of outdated risk assessments [Thames Water, 2023].
  4. Infrastructure breaks down: the drought caused ground movement and widespread bursts in ageing water pipes — producing a record rise in water losses. Asphalt melted on roads and at airports, rails buckled, and major navigable canals (Leeds & Liverpool, Grand Union and others) were closed or subject to navigation restrictions [Thames Water, 2023; Open University; EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)].
  5. Blackout threat: electricity demand rose while generation fell because of cooling problems at thermal and nuclear power plants and low water levels affecting hydropower — in 2022, this ‘nearly caused blackouts’ [Open University].
  6. Pollution: the drought was followed by intense rainfall that severely polluted rivers — the difficulty of treating the water prevented reservoirs from refilling quickly. Company models failed to predict either the speed at which water levels would fall or the obstacles to their recovery [Thames Water, 2023].

3. Financial and economic consequences

  • Collapse of Thames Water: the largest water utility (16 million customers) found itself on the brink of bankruptcy with debt of £16.8 billion; a rescue deal with investors collapsed [Guardian, 2025].
  • Losses in the agricultural sector: the 2022 drought arrived late, allowing winter crops to mature, but potato-sector revenue fell by 6% and sugar-beet production by 18%. The 2025 drought arrived earlier and, according to preliminary data, produced the ‘second-worst harvest on record’: oats −11%, spring barley −8.1%, and barley yields in eastern regions down by as much as 22%.
  • Projected shortfall: England's expected water shortfall by 2055 is 5 billion litres a day, more than one-third of total current consumption [Guardian, 2025]. Summer precipitation will decline by around 15% by the 2050s and by up to 22% by the 2080s [Open University → EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)]; given the acceleration in warming, these levels may be reached 10–15 years earlier.

In winter too: southern England went without water for five consecutive days — freezing weather caused pipes to burst, while Storm Goretti prevented normal water-treatment operations. This was not the first such incident [BBC].

Scotland-2025: the illusion of a ‘safe North’ dispelled

Even in Scotland — one of Europe's wettest regions — the 2025 drought caused levels in reservoirs supplying 300,000 people to fall 40% below the seasonal norm. The region experienced its driest year since 1973 and the 11th-driest start to a year in the 190-year observational record. The water company's management stated directly: ‘if there is another relatively dry winter, more serious supply problems could arise next summer’. The system has lost its safety buffer: it can no longer withstand two consecutive dry seasons, and conditions better than average are required for recovery — a classic sign of a system in deficit.

Conclusion: the crisis in the United Kingdom results from a combination of climate shock, chronic underinvestment and cascading infrastructure failures. All three factors apply to many parts of Europe.

Case study 3: the Colorado River (United States) — a systemic crisis with a predictable endpoint More than 25 years of drought — one of the most severe in the past 1,200 years. Since 2020, average river flow has been 32% below the 20th-century average. The two largest US reservoirs have fallen to record lows: Lake Mead is about 27% full, while Lake Powell is only 23% full. Seven states can no longer agree on who should bear the water cuts. Expand

The Colorado River and its reservoirs have been declining after more than two decades of drought — one of the most severe in the past 1,200 years. In 2026, snowpack in the basin fell to the lowest level on record. Climate change made a snow drought of this severity in the Upper Colorado River Basin approximately 14 times more likely. [Nature Climate Change, 2022Rapid intensification of the emerging southwestern North American megadrought in 2020–2021“2000–2021 was the driest 22-yr period since at least 800.”; PNAS, 2026The 2026 western US snow drought was about four times more likely due to climate change“In the Upper Colorado River Basin, the snow drought was approximately 14 times more likely [0.09, 4,300].”]

Scale: water supplies and hydropower for roughly 35–40 million people, as well as water for 5 million acres of farmland, are at risk across seven US states and Mexico, including Los Angeles, Phoenix and Las Vegas. [Nature Communications, 2025Disentangling climate and policy uncertainties for the Colorado River post-2026 operations“provides water and hydroelectricity for 35–40 million people in seven US states and Mexico”; Los Angeles Times, 2026As Colorado River reservoirs shrink, Arizona warns it could sue“The Colorado River provides water for about 35 million people and 5 million acres of farmland...”]

Consequences of “dead pool”: the reservoir falls to a level at which water can no longer flow through the dam by gravity; hydropower generation has already ceased by that point, and critical water deliveries are disrupted. But the systemic crisis begins long before this physical threshold is reached: the 1922 agreement allocated more water among the states than the shrinking river can now reliably provide. [Los Angeles Times, 2026Colorado River legal fight“The 1922 agreement overpromised what the river could provide.”]

Investor takeaway

The Colorado River crisis is a documented example of systemic failure: climate stress is reducing the physically available resource, the largest reservoirs have reached historic lows, and water scarcity has already escalated into a political conflict between states over who will bear the losses.

Case study 4: Tehran (Iran, 2025–2026) — a capital on the brink of ‘Day Zero’ Water rationing and evacuation were publicly discussed; the authorities lowered water-network pressure at night, while the city's water footprint exceeded the carrying capacity of its water resources. Expand

‘Day Zero’: from anomaly to new normal

The ‘Day Zero’ crises in Cape Town and Barcelona were not random anomalies. Climate models show that these are the first manifestations of a new regime which the Mediterranean region is entering right now; many regions may face a ‘Day Zero’ crisis in the near future [Nature Communications, 2025].

2020s-2030scritical water-shortage crises become an expected risk in the Mediterranean
3.5 yearsaverage drought duration — enough to exhaust the reserves of even a large metropolitan area (the droughts in Barcelona and Cape Town lasted this long)
2 yearsaverage interval between droughts — in 30–50% of cases, rain and meltwater will not be sufficient to replenish reserves before the next drought

Stepwise degradation: when there is not enough time for recovery, each successive drought begins with lower reserves — creating a risk of step-change degradation across the region's entire water system. The region enters a state of permanent water deficit that can be addressed only through extreme and costly measures: permanent water rationing for industry and agriculture, multibillion-euro spending on desalination and water deliveries, and drilling ever-deeper wells.

It is important to interpret the findings correctly: the study does not claim that every city in Southern Europe will run out of water at the same time. It establishes something more fundamental: the entire Mediterranean region is shifting into a new climate regime in which conditions that once produced ‘once-in-a-century’ crises become normal. The baseline operating risk of every water-dependent asset in the region increases manyfold, and crises will become more frequent because further warming intensifies every component: it reduces water inflows while simultaneously increasing consumption.

Investor takeaway

Water is becoming an expensive, scarce and unstable commodity rather than an almost free resource.


Droughts: from manageable risk to systemic shock

The area affected by drought has risen to catastrophic levels not only regionally but globally, directly threatening crops, water supplies and sanitation worldwide.

Global extent (2024) 61% of land was affected by extreme drought (for at least 1 month). This was an absolute record — the area increased by 299% compared with the 1951–1960 average. [Lancet Countdown 2025Lancet Countdown 2025 Global Report“...the percentage of the global land area affected by at least 1 month of extreme drought reached a record-breaking 60·7% in 2024, 299% above the 1951–60 average.”PDF · p. 14]
Prolonged drought (2024) 23% of land experienced more than 6 months of extreme drought. By comparison, in the baseline years (1951–1960), the figure was just 1%. [Lancet Countdown 2025Lancet Countdown 2025 Global Report“23% of the global land area had over 6 months of extreme drought compared with 1% in baseline years.”PDF · p. 14]

Economic damage from droughts, EU + United Kingdom

[EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)PDF · Ch. 11; JRC EDO, 2022]

Past · before ~2010€9 billion/yeara recurring but manageable risk; older assessment models were built on these figures
Now · +1.5 °C€40 billiondamage in 2022 alone — four times the old annual average; the drought covered more than one-third of Europe and was the worst in 500 years for some regions
Future · +3 °C€17.2 billion/yearofficial projection of average annual damage — but actual damage in 2022 has already exceeded the modelled values: the projections probably understate the damage
This is a regime shift, not a percentage increase: the risk has shifted from predictable losses to systemic shocks that exceed even official projections for the future.
DROUGHT DAMAGE, EU+UK · € BILLION 9 average annual damage historical baseline · 1981–2010 40 one year: drought and heat in 2022 actual · Italy, Spain, France 17.2 projected average annual damage at +3 °C · underestimated — actual damage is already higher actual 2022 damage — 2.3 times the +3 °C projection
Diagram 3Jump in drought damage: the single event in 2022 caused four times as much damage as the historical annual average, and 2.3 times as much as the official projection for +3 °C. [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)PDF · Ch. 11]
  • At the peak of summer in 2022, the ‘warning’ drought level affected 47% of EU territory — indicating a clear soil-moisture deficit [JRC, European Drought Observatory, «Drought in Europe — August 2022»].
  • The risk of previously unfamiliar hazards is growing: megadroughts — multiyear events spanning large areas, for which even countries in Central and Northern Europe are unprepared — and rapid-onset droughts (flash droughts), which develop within weeks; existing forecasting and management systems are also unprepared for them [EEA, EUCRA; JRC, World Drought Atlas, 2024].
  • In 2022, drinking water was delivered by tanker to more than 100 French municipalities; restrictions on water use were in force in almost every department of metropolitan France, and local authorities in Italy also restricted water use. In 2018, even Finland and Sweden experienced temporary water shortages [Toreti et al., 2022; EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)].
  • The ‘climate pendulum’: in 2018, drought struck Central and Northern Europe (yields of key cereals fell by as much as 50%, while the harvest increased in the south); in 2022, the pattern was reversed in Southern and Central Europe (EU summer crops: −13–21%). Diversification between ‘south ↔ north’ within Europe offers no protection [JRC, World Drought Atlas, 2024].
  • Price effect: the 2018 crop failure raised soft wheat prices by 34% and barley prices by 48% [EC, 2018; Brás et al., 2021].
  • At +2 °C of warming, 8% of Europe's territory has high or very high sensitivity to desertification [UNEP/UNECE, 2016].
  • By 2050, droughts may affect more than three-quarters of the world's population [UNDRR, GAR, 2025].

Chapter

Energy


04.3.1

The energy sector's water intensity

The power sector is where climate risk and water risk converge: high temperatures and drought simultaneously worsen conditions for hydropower and for most thermal and nuclear power plants.

Water intensity of power generation worldwide

World · Water withdrawals10%of global freshwater withdrawals are used by the energy system [WWF, 2023]
World · Cooling~90%of global electricity generation is water-intensive (primarily because thermal and nuclear power plants require cooling) [WWF, 2023]
World · Hydropower generation~15%of global electricity generation comes from hydropower [WWF, 2023]

Water intensity of power generation in Europe

Europe · Consumption37%of total water consumption in Europe is attributable to the energy sector (some of the water is returned to water bodies after use) [EEA, 2024]
Europe · Cooling65%of electricity generation in Europe depends on water for cooling [EEA, 2024]


04.3.2

Already happening

2026 — Danube: In Hungary, the Paks nuclear power plant, which normally supplies around half of the country’s electricity, was operating at about 10% of capacity. In Romania, one of the two reactors at the Cernavodă nuclear power plant, which normally supplies around 20% of the country’s electricity, was shut down because of low Danube levels. Losing one reactor reduced national generation by roughly 10%. Both countries had to increase electricity imports and urge consumers to reduce demand. [Reuters, 2026Reuters — Hungary PM flags 'critical' days ahead with looming nuclear shutdown“Paks power plant, which generates about half of the country's electricity, was running at just over 10% of its capacity...”Web · 2 August 2026 / Reuters, 2026Reuters — Romania races to divert Danube water as Hungary's Paks runs on last turbine“normally generates a fifth ... shut down one of its two reactors...”“forcing Budapest and Bucharest to increase power imports and urge households and businesses to reduce consumption.”Web · 4 August 2026]

During Spain's 2022 drought, hydropower generation fell by 48%; during the extreme heat of 2003, French nuclear power plants lost up to 25% of their capacity. In 2022–2025, nuclear and thermal power plants in Switzerland and France were forced to shut down because their cooling water was too warm, causing wholesale energy prices to triple [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024); WRI].

European generation losses: thermal and nuclear power

NowSouthern Europe's energy system already faces risks [EEA, 2024].

For nuclear power plants, average annual losses from drought are around 1%, rising to 5% in extreme cases [JRC, 2023].
+2 °CAvailable capacity at river-cooled power plants declines by around 10% [MedECC, 2020].
+3 °CCapacity declines by ~15% in most countries (and by 15–20% in Bulgaria, Greece and Spain) [MedECC, 2020].

In France, losses may increase by a factor of 2–3 [JRC, 2023].

European generation losses: hydropower

NowSouthern Europe loses up to 10% of generation (Portugal, Cyprus, Spain and Greece are hit hardest) [JRC, 2023].
+2 °CIn the most vulnerable countries (Greece, Portugal and Spain), hydropower potential declines by less than 10% [MedECC, 2020].
+3 °CA decline of 15–20% in Greece, Portugal and Spain [MedECC, 2020].

Losses may double or triple [JRC, 2023].

04.3.3

Cascade

The cumulative effect of a climate shock (heat and drought) puts the energy system under pressure on two fronts: supply falls at the same time as energy demand rises sharply. This creates a threat of cascading outages (blackouts) and price destabilisation.

DROUGHT + HEAT one climate shock Generation FALLS: hydro (less water); nuclear/thermal (less effective cooling) Demand RISES: peak air-conditioning demand in hot weather PRICE SPIKES rolling outages, threat of a blackout
Diagram 4A ‘perfect storm’ for the energy system: the same shock simultaneously reduces supply and increases demand. [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024); WRI]

04.3.4

Grid risk: power transmission

Heat affects not only power plants but the grid itself. Failure rates often increase when surface temperatures exceed 30 °C. In the British assessment of energy-system vulnerability, grid assets are identified as the most vulnerable category [DESNZ, 2025UK Department for Energy Security & Net Zero — Impacts on energy assets from extreme heat and heatwaves"Overall, the most vulnerable asset category was power sector networks.""Historical analysis of extreme heat and the electricity system demonstrated that faults have often increased in frequency when surface temperatures exceed 30 °C."PDF · p. 5].

Cables, transformers and grid equipment become hotter or dissipate heat less effectively, causing them to become less efficient, wear out faster or shut down [DESNZ, 2025UK Department for Energy Security & Net Zero — Impacts on energy assets from extreme heat and heatwaves"Underground cables were identified as ‘vulnerable’ ... Extreme temperatures can prevent efficient heat dissipation.""Transformers were identified as ‘vulnerable’ ... extreme temperatures prevent efficient heat dissipation, accelerates insulation degradation, affecting capacity and shortening lifespan."PDF · pp. 33–34].

Weather-related outages are already becoming more frequent. In the United States, there were approximately 60% more major outages during the hot season in 2014–2023 than in 2000–2009. [Climate Central / DOE Form OE-417Climate Central — Heat Season Power Outages"The U.S. experienced about 60% more heat season power outages during the last 10 years (2014-2023) than during the first 10 years analyzed (2000-2009).""Heat season outages accounted for nearly half (47% or 831) of all 1,755 weather-related outages during the 2000-2023 period."Website · data: U.S. Department of Energy Form OE-417] 62.1% of prolonged outages lasting 8+ hours in the United States coincided with extreme weather or climate events. [Nature Communications, 2023Spatiotemporal distribution of power outages with climate events and social vulnerability in the USA"62.1% of 8+ hour outages co-occur with extreme weather/climate events, particularly heavy precipitation, anomalous heat, and tropical cyclones.""8+ hour outages are 3.4x more common on days with a single event and 10x more common on days with multiple events."Article · Results]

Distribution grids in Europe are also becoming increasingly exposed to risk: extreme weather already causes significant damage to grid operators, and that damage is expected to grow rapidly. [Eurelectric, 2025Eurelectric — Strengthening climate resilience"As the damage caused by extreme weather events on grid operators, already significant in 2025, is expected to increase massively, taking actions to enhance resilience is not an option anymore."PDF · p. 2]

This applies primarily to traditional centralised grids. Decentralised energy systems (hybrid solar plants, storage and microgrids) can operate autonomously — even when the main grid suffers a failure. [DOE, 2024U.S. Department of Energy — Microgrid Overview"The primary resilience benefit of microgrids is their ability to disconnect from the main grid when there is an outage and operate autonomously.""Facilities connected to and powered by the microgrid can continue serving a community during an outage."PDF · p. 2] [NREL, 2019National Renewable Energy Laboratory — Power Sector Resilience"Systems that are designed to operate in islanded mode can be isolated from a larger grid, allowing the system to generate and distribute energy on-site in the event of a power outage.""Microgrids are often implemented where on-site renewable energy is combined with energy storage to support resilience."PDF · p. 1]

Investor takeaway

Thermal and hydropower assets in areas of water stress require an additional discount and stress testing. With their minimal water footprint, solar and wind power are becoming not only a carbon hedge but also a water hedge for the energy system — a hidden resilience advantage under scenarios of +2 °C and above.

Chapter

Food

Food-system vulnerability: The stable climate that sustained reliable harvests for generations is now in the past. We are entering an era of chaotic weather in which droughts, floods and heatwaves reduce crop yields and may strike several of the world’s breadbaskets at once.

Illusion of safety: Countries that consider themselves protected from climate risk may be critically dependent on food imports from the most vulnerable regions.

Social consequences: The climate crisis is already driving up food prices. Experts warn that more expensive food could heighten tensions, potentially leading to civil unrest.

04.4 Food

Food-system vulnerability

The food system depends on temperature conditions, water resources and outdoor labour. Heat, moisture deficits and extreme rainfall put pressure on all these pillars at once. This is a systemic risk to global food security and to the 1.23 billion people who depend on agriculture [FAO/WMO, 2026]FAO/WMO — Extreme heat and agriculture (2026)“Extreme heat magnifies existing weaknesses across agricultural systems... These impacts extend far beyond the farm gate. They represent a systemic risk...”“...the livelihoods of more than 1.23 billion people who rely on agriculture.”PDF · p. 9.


Declining crop yields

Every additional degree of global warming reduces the yields of the main crops that provide 60% of global calorie consumption. The figures below show the average effect per +1 °C: once temperatures exceed a crop’s optimum, the decline becomes non-linear and accelerates [FAO/WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“the negative impacts associated with high temperature on the productivity of the major grains that supply 60 percent of global caloric food intake (maize, rice, soy, wheat)”“At temperatures above the optimal temperature threshold, a non-linear decline in development is observed...”PDF · pp. 18–19]:

MaizeRiceSoybeanWheat
Decline in crop yields per +1 °C −7,5% [FAO/WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“Averaged globally ... annual crop yields are reported as -7.5 percent ... for maize, -1.2 percent ... for rice, -6.8 percent ... for soybean and -6.0 percent ... for wheat per 1 °C of warming.”PDF · pp. 18–19] −1,2% [FAO/WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“Averaged globally ... annual crop yields are reported as -7.5 percent ... for maize, -1.2 percent ... for rice, -6.8 percent ... for soybean and -6.0 percent ... for wheat per 1 °C of warming.”PDF · pp. 18–19] −6,8% [FAO/WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“Averaged globally ... annual crop yields are reported as -7.5 percent ... for maize, -1.2 percent ... for rice, -6.8 percent ... for soybean and -6.0 percent ... for wheat per 1 °C of warming.”PDF · pp. 18–19] −6,0% [FAO/WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“Averaged globally ... annual crop yields are reported as -7.5 percent ... for maize, -1.2 percent ... for rice, -6.8 percent ... for soybean and -6.0 percent ... for wheat per 1 °C of warming.”PDF · pp. 18–19]
Heat and moisture deficit combined
−24,89%
yield loss when heat coincides with a moisture deficit — almost three times the loss caused by high temperatures alone [FAO/WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“losses from combined heatwaves and low precipitation were observed to be nearly triple at 24.89 percent.”PDF · p. 19]

Climate threatens every pillar of production: crop yields, labour and land:


Risk at +2…+3 °C

At +2 °C10–31%of current production of major crops would fall outside the climatically suitable range in regions critical to food supply (South Asia, the Middle East and North Africa, sub-Saharan Africa, Southeast Asia, Central America and parts of South America). The range of crops suitable for cultivation narrows across 52% of global cropland [Nature, 2025Climate change threatens crop diversity at low latitudes (2025)“We found that in low-latitude regions, 10–31% of current production would shift outside the climatic niche even under 2 °C global warming, increasing to 20–48% under 3 °C warming.”“potential food crop diversity would decline on 52% (+2 °C) and 56% (+3 °C) of global cropland.”PDF · p. 1]
The main jump in risk already occurs between +2 °C and +3 °C — at levels to which current policy leads; +4 °C merely takes the picture to its limit.

At the same time, the impacts of +2 °C warming could be substantially more severe, as projections at +2 °C vary widely: around a quarter of climate models project stronger droughts across the world’s breadbasket regions at +2 °C than the average estimates for +4 °C [Nature, 2026Bevacqua et al. - Moderate global warming does not rule out extreme global climate outcomes (2026)“Out of 42 models, 10 models show climate outcomes at a 2 °C warming that are well beyond the multimodel mean at 4 °C of global warming.”].


At +4 °C, the greatest losses are not in poor countries but in rich ‘breadbaskets’

It is widely assumed that climate-driven hunger is a problem for poor countries. The calculations show otherwise: the decline in food-calorie production follows a U-shaped pattern by income. The largest losses occur both in the poorest regions (because they depend on vulnerable crops, especially cassava) and in the richest, where modern ‘breadbaskets’ with high yields but limited current adaptation to heat are concentrated [Impacts of climate change, 2025Impacts of climate change on global agriculture (2025)“global impacts are dominated by losses to modern-day breadbaskets with favourable climates and limited present adaptation.”“We estimate average losses of 28% in the lowest-income decile but more moderate losses of roughly 18% across deciles 2–8. In the highest-income deciles, average losses increase to 29% (ninth) and 41% (top).”PDF · p. 5].

The estimates relate to a high-emissions scenario (RCP 8.5, warming of around +4 °C, by the end of the century) and are compared with a world without climate change. Importantly, this is not a single-day event, but a trend showing the scale of a process already under way. Losses build gradually as temperatures rise. Referring to ‘+4 °C’ or ‘2100’ is merely a model checkpoint. With the current acceleration of climate change, this level could be reached significantly earlier.

Highest-income 10% (by income)−41%of calorie production is lost in the world’s key ‘breadbaskets’ (the richest regions) — more than in any other income group [Impacts of climate change, 2025Impacts of climate change on global agriculture (2025)“In the highest-income deciles, average losses increase to 29% (ninth) and 41% (top).”PDF · p. 5]
Yield losses are concentrated in developed agricultural regions to which Western portfolios are tied; adaptation eliminates only about one-third of the damage.

Wheat: the area suitable for cultivation shrinks

At +4 °C the climatically suitable area for rainfed wheat — one of the world’s key food crops — declines, very unevenly across regions. This is a guide to the warming level, not a calendar date: the process is already under way, and with the current acceleration this level could be reached earlier [FAO, SOLAW, 2025FAO — SOLAW 2025 (Table 9, SSP 8.5, 2081–2100)“Under the SSP 8.5 scenario and with an assumption of advanced management conditions in place, projections indicate a net increase in suitable areas for cassava, maize and soybean, but an overall reduction for wheat.”“SSP5-8.5 … Warming (best estimate) (2081–2100) 4.4 °C (very likely range 3.3–5.7 °C).” (Table A.1)PDF · p. 68; Table A.1, p. 130].

World−10%of the area suitable for wheat at +4 °C — the only one of the four staple crops (cassava, maize, soybean and wheat) to lose area globally [FAO, SOLAW, 2025FAO — SOLAW 2025 (Table 9)WORLD wheat: historical 799.9 Mha; SSP 8.5 variation −10.2%.PDF · p. 68]
Climate shifts the very map of where crops can be grown: the north gains suitable land, while the tropics and subtropics lose it.

For cassava, maize and soybean, the same calculations show an increase in suitable area — but this is ‘maximum potential under ideal conditions, not an actual outcome’: more suitable area does not mean higher yields if climate stresses limit productivity even on newly suitable land [FAO, SOLAW, 2025FAO — SOLAW 2025“This does not necessarily imply higher production of the three aforementioned crops, as the scenarios do not take into account extreme events and socioeconomic factors; the analysis shows the maximum potential, not actual outcomes, under the assumption of ideal biophysical and socioeconomic conditions.”“increased suitable land does not always correlate with increased productivity ... especially if climate stressors limit yields even in newly suitable areas.”PDF · pp. 69–70].


A physical limit

The food system is running up against a physical limit — land scarcity. Expanding agricultural land is no longer viable [FAO, SOLAW, 2025FAO — The State of the World’s Land and Water Resources (SOLAW 2025)“...the potential for agricultural expansion is limited, as further land conversion to cropland would impact other ecosystems, including forests, grasslands and wetlands.”PDF · p. xiv (16); FAO Newsroom, 2025FAO Newsroom — SOLAW 2025 press release“Expanding agricultural area is no longer viable, the report stresses.”FAO Website]. At the same time, population growth requires annual increases in production [FAO, SOLAW, 2025FAO — The State of the World’s Land and Water Resources (SOLAW 2025)“By 2050, the global population is projected to reach 9.7 billion, and agriculture will need to produce around 50 percent more food, feed and fibre than in 2012.”PDF · p. vi (8); FAO Newsroom, 2025FAO Newsroom — SOLAW 2025 press release“...requiring agriculture to produce 50 percent more food, feed and fibre than in 2012, alongside 25 percent more freshwater.”FAO Website]. Without radical changes to agricultural technology and diets, land demand will exceed supply even in a stable climate. The systemic decline in crop yields caused by global warming further aggravates this crisis.

Land becomes a separate constraint on the food system: new land requires deforestation, existing land degrades, and livestock ties up a large share of the resource.

Climate pressure is superimposed on an already depleted land base: more than 1,660 million ha of land (more than 10% of all land on Earth) has already been degraded, and more than 60% of this degradation is on agricultural land [FAO, SOLAW, 2025FAO — The State of the World’s Land and Water Resources (SOLAW 2025)“More than 1 660 Mha of land, corresponding to more than 10 percent of the world’s land area, have been degraded by unsustainable land-use and management practices, with more than 60 percent of this degradation occurring on agricultural lands (including cropland and pastureland).”PDF · p. xvi (16)].

Salinisation: irreversible loss of arable land

Sea-level rise and groundwater depletion lead to saltwater intrusion in coastal regions. This process renders vast areas of formerly fertile land unsuitable for agriculture. In 2022, in the Po River delta — one of Europe’s most productive agricultural regions — saltwater penetrated a record 40 km inland [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)]. Salinisation alone has already degraded 82 million ha of rainfed and 24 million ha of irrigated cropland [FAO, SOLAW, 2025FAO — The State of the World’s Land and Water Resources (SOLAW 2025)“Conservative estimates of the impact of soil erosion and salinization indicate that 82 Mha of rainfed cropland and 24 Mha of irrigated cropland are degraded from salinization processes alone (FAO, 2024a).”PDF · p. 29].


Water limit: irrigation as a hidden balance-sheet risk

Food security depends substantially on a water resource that is becoming scarcer. Rather than adapting, the global economy is expanding production through irrigation where water resources are already under stress. Reliable irrigation can support crop yields, but amid groundwater depletion and competition for water from cities, energy and industry, it becomes a source of risk.

The most productive agricultural regions depend on irrigation — and therefore on water reserves that are being depleted. The dependency is concentrated: the bulk of irrigated food is produced where water is already scarce.

Investor takeaway

Irrigation systems, agricultural land and processing operations without a reliable water supply may look like productive assets, but in essence they depend on a resource that is physically being depleted.


Prices: a local shock goes global

Global production is often concentrated in a few regions, partly because those locations have the best natural conditions for particular crops. A climate shock to one region can therefore cause shortages or price rises worldwide. The current pace of climate change means that conditions to which agriculture is adapted will be disrupted ever more often [Kotz et al., 2025]Kotz et al. — Climate extremes, food price spikes, and their wider societal risks (2025)“With current policies and actions set to lead to global warming of between 2.2 °C and 3.4 °C above pre-industrial levels, unprecedented conditions are set to become increasingly common across the world.”“At the same time, new records for extreme conditions will continue to be set, further from those to which agricultural production and economic systems are currently adapted.”PDF · p. 4.

Case study: United Kingdom

In the report ‘Global biodiversity loss, ecosystem collapse and national security’ (2025) UK intelligence highlights the vulnerability of the country’s food system to climate and environmental shocks [HM Government, 2025Global biodiversity loss, ecosystem collapse and national security (2025)“Ecosystem degradation or collapse will challenge the UK’s food security... The UK imports 40% of its food from overseas... The UK is unable to be food self-sufficient at present, based on current diets and prices.”PDF · p. 10]:

  • The United Kingdom’s critical dependence on imports: The country imports 40% of its food and 18% of livestock feed (soy from South America); almost 50% of packaged products contain imported palm oil. It also depends on imported fertiliser.
  • The impossibility of self-sufficiency: The United Kingdom does not have enough land to feed its population and livestock. Full self-sufficiency with current diets is impossible — it would require a radical dietary shift and a huge increase in prices.
  • Vulnerability to global shocks: A collapse in production in two or more global ‘breadbaskets’ would cause unpredictable price rises. This would limit the country’s ability to import food, prompt government intervention in supply chains and trigger conflicts over food.
  • Domestic threats: Domestic agricultural production is already threatened by soil depletion, loss of pollinators, droughts and floods.

Synchronous shocks: multiple breadbaskets at once

Heat and drought increasingly create a risk of simultaneous shocks to several agricultural regions: in the mid-latitudes of the Northern Hemisphere, the frequency of concurrent heatwaves has increased approximately 6-fold over 1979–2019. [FAO & WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“concurrent heatwaves ... across the mid-latitude regions (30° to 60° North) in the Northern Hemisphere between 1979–2019”“an approximately 500 percent (or six-fold) increase in their frequency”PDF · p. 7]. The risk of ‘synchronised crop failure’ is growing: persistent Rossby waves can cause extreme heat simultaneously in key agricultural regions of North America, Europe and Asia. For the most severe events, the likelihood of such concurrent extremes increases by a factor of up to 20. [Kornhuber et al., 2020Nature Climate Change — Amplified Rossby waves enhance risk of concurrent heatwaves in major breadbasket regions“Those patterns can induce simultaneous heat extremes in specific regions: Central North America, Eastern Europe and Eastern Asia for wave 5, and Western Central North America, Western Europe and Western Asia for wave 7.”“The probability of simultaneous heat extremes in these regions increases by a factor of up to 20 for the most severe heat events...”PDF · p. 1].

If several key producing regions — ‘breadbaskets’ — are hit by climate shocks simultaneously, the global market may respond with food-price spikes, threatening global food-market stability and food security. [IFPRI / CGIAR, 2025Global Food Security Impacts of Extreme Weather Events and Occurrence of Breadbasket Failures“...multiple breadbasket failures have happened in the past and are expected to pose major threats to global food market stability and food security...”“...synchronized agricultural losses, reducing food availability and driving up food prices, thus undermining food security...”PDF · p. 16]. Countries and regions dependent on food imports are particularly vulnerable. [IFPRI / CGIAR, 2025Global Food Security Impacts of Extreme Weather Events and Occurrence of Breadbasket Failures“These conditions underscore the critical role of global trade in shaping domestic food prices and food security.”“...particularly vulnerable to crop failures not just within their own borders or regions but also in major crop-exporting countries elsewhere in the world.”PDF · p. 16].

This is not only a risk of synchronous pressure on different countries. A single season of climate shocks can simultaneously disrupt several regions within one country, affecting different production channels: water, crop yields, livestock, wildfires, labour productivity and logistics [FAO & WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“...extreme heat is a major risk multiplier, exerting mounting pressure on crops, livestock, fisheries and forests...”“The full danger of extreme heat lies not only in its direct impacts, but also in its role as a risk multiplier, amplifying the effect of water stress, serving as a trigger of flash droughts and elevating the risk of wildfires...”PDF; Malik et al., 2022Nature Food — Impacts of climate change and extreme weather on food supply chains cascade across sectors and regions in Australia“Disruptions caused by extreme weather events can cascade across regions and sectors, resulting in job and income losses and impacts on food availability.”Article · Nature Food].

Climate change therefore acts as a geopolitical threat multiplier: local agronomic problems can turn into market, social and political crises, while conventional diversification ‘by region’ loses some of its protective value. [FAO & WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“This work highlights how extreme heat is a major risk multiplier...”“More than simply an isolated climatic hazard, it acts as a compounding risk factor that magnifies existing weaknesses across agricultural systems.”PDF; Kornhuber et al., 2020Nature Climate Change — Amplified Rossby waves enhance risk of concurrent heatwaves in major breadbasket regions“As these regions are important for global food production, the identified teleconnections have the potential to fuel multiple harvest failures, posing risks to global food security.”PDF · p. 2].

Case study: Brazil — heat and downpours hit two crops at once Soybean: harvest forecast cut from 162 to 147.7 million tonnes. Rice: productivity fell after flooding in the state that produces more than 70% of Brazil’s supply. Expand

Brazil illustrates why food risk cannot be treated as a single type of disaster. In the 2023–2024 season, prolonged heat hit soybeans: CONAB’s national forecast was cut from 162 to 147.7 million tonnes, almost 10%, and soybean-yield losses in São Paulo were estimated at more than 20%. Flooding in Rio Grande do Sul, which produces more than 70% of Brazil’s rice, then reduced rice productivity and destroyed up to 2 million tonnes of soybeans [FAO/WMO, 2026FAO/WMO — Extreme heat and agriculture (2026)“Initial forecasts from Brazil's National Supply Company, CONAB ... projected a record crop of 162 million metric tonnes. However ... by May 2024, the estimate was slashed to 147.7 million metric tonnes, a reduction of nearly 10 percent.”“For example, the reduction in soy yield was estimated to be more than 20 percent in the state of São Paulo.”“Rio Grande do Sul, which accounts for over 70 percent of Brazil's rice output, saw productivity reduced by 3.6 percent over the previous harvest.”“The flood led to the destruction of up to 2 million tonnes of soybeans.”PDF · pp. 62, 68].


Price rises can lead to hunger and social conflict

Investor takeaway

Climate pressure on agriculture creates a systemic cascading risk. The physical limit on arable land means that falling crop yields cannot be offset by bringing ever more land into production, turning this shortage into a long-term systemic driver of structural inflation and macroeconomic destabilisation.

Chapter

Wildfires

Climate change is turning megafires from rare anomalies into a new regular occurrence. Asset destruction and smoke pollution create major economic costs.

04.5 Wildfires

From local disasters to systemic risk

Climate change has significantly increased the likelihood of extreme fire-weather conditions (FWI) in the Mediterranean:

Worldwide, the number of days per year with fire-prone conditions has almost tripled since the 1980s [Nature, 2026Increasing synchronicity of global extreme fire weather“The number of days per year with fire-prone conditions has nearly tripled globally since the 1980s...”Nature Ecology & Evolution]. What used to happen once every 100 years before climate change now occurs every 10–18 years. At +2.6 °C of warming, such extreme fire-weather conditions will occur almost every year [WWA, 2025World Weather Attribution (2025)“The event in today's climate is about a 1 in 10 year event, whereas in a 1.3°C cooler climate, it would be expected to occur once in every 100 years. ... The DSR is projected to become another 25% more intense and another nine times more likely.”PDF · p. 3].

The growing number of major wildfires causes significant damage and spreads smoke, creating serious air-quality problems even far from the source [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)]. This also means direct economic losses (timber, infrastructure and tourism) and long-term ecological damage that undermines forests’ ability to absorb CO₂.


Future projections

Climate model estimates vary widely, and warming could have a substantially greater effect. The four models with the most severe projections show more extreme fire-weather conditions across the world’s forests at +2 °C than the average projection for +3 °C. The highest and lowest estimates at +2 °C differ by more than a factor of four [Nature, 2026Bevacqua et al. - Moderate global warming does not rule out extreme global climate outcomes (2026)“The four worst-case models at a moderate 2 °C warming show an increase in FWI extremes across forests larger than the multimodel mean projection at 3 °C warming...”“...the worst-case model showing an increase more than 4-times larger than the best-case model (+6.5 against +1.5 relative to preindustrial conditions...)”].

Investor takeaway

Wildfires have evolved from one-off force majeure events into a predictable systemic risk. The cumulative impacts of infrastructure destruction, a catastrophic deterioration in air quality and insurers withdrawing from ‘red zones’ make it essential to include wildfire indices when assessing the long-term resilience of assets and property portfolios.

Chapter

Flooding

Flood risk in Europe is rising significantly. Losses from a single event can reach double-digit shares of GDP, creating a direct threat of sovereign default.


04.6 Flooding

Flooding: losses from one event as a share of national GDP

Flood risk in Europe is rising significantly. For Central and Western Europe, it is the principal climate risk: floods account for 50% of all weather-related losses [Swiss Re, 2024]. Without additional protection, annual damage from coastal flooding alone could exceed €1 trillion by the end of the century.

€170 billionflood damage in Europe over the past 30 years[EEA, EUCRA, 2025EEA — European Climate Risk Assessment, EUCRA]
€44 billiona single flood in Germany and Belgium in July 2021 — one-quarter of all damage over the preceding 30 years[EEA, EUCRA, 2025EEA — European Climate Risk Assessment, EUCRA]
7–17% of GDPgovernment financial liabilities from ‘once-in-a-century’ floods[EEA, EUCRA, 2025EEA — European Climate Risk Assessment, EUCRA]

Land subsidence compounds flood risk in coastal megacities: the land sinks towards the rising sea. In England, where every degree of warming allows the atmosphere to hold about 7% more water vapour, 6.3 million homes are already in areas at risk of flooding from rivers, the sea or surface water [Euronews, 2025].


Future projections

At +2 °C, extreme five-day precipitation in densely populated areas increases by 4-15% relative to the pre-industrial climate, depending on the model. The most severe projections at +2 °C already exceed the average projection for +3 °C [Nature, 2026Bevacqua et al. - Moderate global warming does not rule out extreme global climate outcomes (2026)“In a 2 °C world, heavy precipitation projections over populated areas vary widely across climate models, ranging from an increase of 4% to 15%.”“The worst-case climate outcome is particularly extreme, with precipitation extremes across populated areas at a moderate 2 °C warming projected to exceed the multimodel mean at 3 °C of global warming.”].

Investor takeaway

The intensity and financial consequences of flooding are rising sharply; a single event can create liabilities equivalent to a share of a country’s annual GDP. Mutual-aid mechanisms (EUSF) are already operating at their limit — the next trigger could be systemic.

Hurricanes and storms

Hidden burden: official statistics capture only a small fraction of the losses.

A decade-long legacy: the consequences of storms extend over a decade.

Systemic driver: hurricanes are one of the largest unaccounted drivers of mortality.

04.7 Hurricanes and tropical storms (the US example)

The hidden cost of extreme weather events

A recent study of excess mortality after tropical cyclones in the continental United States (1930–2015) found that the conventional approach to counting losses radically understates their true scale [Nature, 2024Nature — Mortality caused by tropical cyclones in the United States (2024)“we estimate that the average TC indirectly accelerated the death of roughly 7,170–11,430 individuals... This burden is 300–480 times greater than government (NOAA) estimates”PDF · pp. 3, 5].

Overall conclusion

Hurricanes and tropical storms are not merely short-lived shocks, but systemic drivers of long-term excess mortality. The absence of evidence of autonomous adaptation over almost a century of observations indicates that current response strategies are insufficient to protect people from growing risks.

Chapter

Sea-level rise

Seemingly the slowest-moving yet irreversible climate risk. The financial impact arrives long before the water rises — through the repricing of coastal assets by markets, insurers and banks.


04.8 Sea level

The core problem: the water keeps rising and does not recede

The ocean is warming and expanding, and melting glaciers add even more water — causing sea level to rise [NASA, 2024Hamlington et al. — The rate of global sea level rise doubled during the past three decades (2024)"The ocean has absorbed about 90% of the extra heat trapped by the atmosphere, leading to an expansion in ocean waters as it warms."PDF · p. 1]. The process is nearly irreversible over generational timescales: part of the future rise is already ‘locked in’ today and will continue for centuries even if emissions stop [Royal Society, 2026Millman, Siegert, Alley — The achievability of low-emission IPCC sea-level rise scenarios (2026)"approximately 30 cm of additional sea-level rise is already committed from the Greenland Ice Sheet."PDF · p. 2].

A direct consequence of sea-level rise is the growing risk of permanent inundation or storm-surge flooding along densely populated low-lying coastlines and in major coastal cities. This threatens cities such as Shanghai, Miami, New York, Alexandria, New Orleans, Tokyo, Mumbai, Osaka–Kobe, Guangzhou, Ho Chi Minh City, Kolkata, Tianjin, Bangkok, Dhaka and Hai Phong [OECD, Ranking Port Cities with High Exposure, 2008OECD Environment Working Papers"Top 20 cities in all the rankings include Mumbai, Guangzhou, Shanghai, Miami, Ho Chi Minh City, Kolkata, New York, Osaka-Kobe, Alexandria, New Orleans, Tokyo, Tianjin, Bangkok, Dhaka and Hai Phong."PDF · p. 8]. More than 150 million people live less than 1 m above sea level — directly exposed to flooding [Lancet Countdown, 2025The 2025 report of the Lancet Countdown on health and climate change"in 2024, 156·7 million people were living less than 1 m above current sea levels as of December, 2024""Between 1993 and 2023, the global average sea level rose by 101·4 mm and is projected to continue rising."PDF · p. 24].

At the same time, protecting most of the coast is not economically viable — investment pays off along only about 13% of the world’s coastline; the rest faces managed or unmanaged retreat.[Nature Sustainability, 2026Molino et al. — Sea-level-driven land conversion amplified by coastal agriculture (2026)"traditional economic metrics justify the protection of only 13% of the global coastline."PDF · p. 5].

New York shows that this is no longer a distant scenario: the city has more than 500 miles of shoreline, and sea-level rise already threatens waterfront neighbourhoods in all five boroughs. The number of days with tidal flooding in New York rose by 200% between 2000 and 2021, while much of the shoreline remains without comprehensive protection. Just one project to protect Lower Manhattan and the Seaport district is estimated at $5.5 billion in 2025 prices and could rise to $8–9 billion by the time construction begins; the city explicitly identifies funding as the main remaining barrier [NYC Health, 2024New York City Department of Health and Mental Hygiene"Data show that there was a 200% increase in high tide flood days from 2000 to 2021.""The sea level in NYC is rising, which makes powerful storm surges worse."Website; NYC Comptroller, 2019Safeguarding Our Shores"With more than 500 miles of coastline, New York City sits on the frontlines of climate change.""Rising sea levels already threaten the safety of our shorefront communities across all five boroughs.""much of our coastline remains unprotected from the next storm."PDF · p. 3; NYC FiDi-Seaport Climate Resilience Plan, 2025Implementation"The estimated capital cost of the FiDi-Seaport Climate Resilience Plan is $5.5 billion in 2025 dollars.""with escalation, the total project cost will be an estimated $8-9 billion.""the biggest barrier that remains is funding."Website].

The rise is already under way — and accelerating

Underestimating the risk

Official projections represent the lower bound of the risk range. Observations show that sea-level rise is happening faster than projected, while ice-sheet models underestimate the pace of break-up — so official projections are likely to understate future rise [Royal Society, 2026Millman, Siegert, Alley — The achievability of low-emission IPCC sea-level rise scenarios (2026)"Observations suggest we are currently tracking sea-level rise pathways consistent with intermediate- to high-emission scenarios... projections may underestimate the true pace and magnitude of future sea-level rise."PDF · p. 12].

The ‘global’ figure understates local risk. Because of land subsidence and ocean currents, sea level is rising twice as fast as the global average along some coastlines — for example, along the Atlantic coast of the United States [Nature Sustainability, 2026Molino et al. — Sea-level-driven land conversion amplified by coastal agriculture (2026)"the mid-Atlantic coast represents a known hotspot of global SLR, with RSLRR double the global average."PDF · p. 6].

Damage occurs before flooding

Investor takeaway

Sea-level rise is a physically irreversible process whose impacts — stronger storm surges, coastal erosion and freshwater salinisation — are already damaging coastal infrastructure and agriculture. Asset degradation and rising spending on coastal protection begin long before land is submerged.

Chapter

Biodiversity

Foundation of the economy: Biodiversity is not just nature; it is the basic infrastructure for humanity’s survival. Pollinators, soil formation, pest control and the water cycle all depend on complex ecosystems.

Systemic collapse: Biodiversity loss has moved from the environmental agenda into the national security domain. Key ecosystems are on the brink of collapse, threatening to trigger cascading shocks across the global economy.


04.9 Biodiversity


A problem with catastrophic potential

Biodiversity — is the variability among living organisms from all sources, including terrestrial, marine and other aquatic ecosystems and the ecological complexes of which they are part.

Biodiversity and nature’s contributions to people underpin the economy, so all businesses depend on biodiversity, directly or indirectly. Biodiversity loss is no longer solely an environmental problem; it has become a systemic risk threatening the entire global economy, financial stability and human well-being [IPBES, 2026IPBES Business and Biodiversity Assessment Summary for Policymakers“Biodiversity and nature's contributions to people underpin the economy, so all businesses depend, directly or indirectly, on biodiversity... The decline in biodiversity... has become a critical systemic risk threatening the economy, financial stability and human wellbeing”PDF · p. 5]. The degradation of nature is classified as a factor capable of undermining the foundations of the global economy and geopolitical stability.

Diverse species and habitats provide clean air and water, fertile soils and pollination, supporting food security, livelihoods and health, regulating the climate and protecting against extreme events. Climate change is one of the main causes of biodiversity degradation [ESOTC, 2025European State of the Climate (ESOTC) 2025“Diverse species and habitats support clean air and water, fertile soils and pollination, contributing to food security, livelihoods and health... regulate the climate and protect against extreme events. Climate change is a major cause of its degradation.”PDF · p. 9]. At the same time, climate change and biodiversity loss reinforce each other in destabilising ways [10NICS, 202510NICS (2025)“Mounting evidence shows that climate change and biodiversity loss reinforce each other... 3–6 million (or more) animal and plant species are threatened, even under intermediate climate change scenarios.”].

Climate change is causing species to lose part of their climatically suitable range — the area where conditions remain suitable for them to live and reproduce. The tables below show the share of species that could lose more than half of that range. [Price et al., 2024 / Warren et al., 2018Biodiversity losses associated with global warming of 1.5 to 4 °C“At 2 °C, these projections of loss fall to 18% of insects, 16% of plants and 8% of vertebrates...”“...for warming of 3.2 °C... ~49% of insects, 44% of plants and 26% of vertebrates...”Article · review of the estimate by Warren et al., 2018].


Humanity in ecological overshoot

Global economic growth over recent centuries was paid for with ecological capital. The global economy is in a state of ‘advanced ecological overshoot’, where the scale of human pressure exceeds the planet’s capacity to regenerate.

Resource deficit 160% of the planet’s available resources are consumed by humanity each year. We are depleting renewable natural capital faster than it can regenerate, accumulating ecological debt [HM Government, 2025Global biodiversity loss, ecosystem collapse and national security (2025)“Nature is a finite asset which underpins the global economy. It would take resources of 1.6 Earths to sustain the world's current levels of consumption.”PDF · p. 9].
Absolute dominance96%of all mammalian biomass on Earth consists of humans (32%) and their livestock (64%). Wild animals account for just 4%. Human-made mass has already surpassed the planet’s entire living biomass [The Human Ecology of Overshoot, 2023The Human Ecology of Overshoot (2023)Of mammalian biomass, humans account for 32%, livestock for 64% and wild mammals for 4%. Human-made mass has surpassed living biomass (~1.1 teratonnes).].

The degradation of nature is a macro-risk

The economic impact of nature loss could equal that of the 2008 financial crisis or the COVID-19 pandemic within the next 10 years [Tipping into the wild unknown, 2026IFoA & Anglia Ruskin University — Planetary Solvency: Tipping into the wild unknown (2026)"a material risk of biodiversity and nature-related macroeconomic impacts equalling the 2008 Global Financial Crisis, or even the Covid-19 pandemic, within the next 10 years."PDF · p. 29]. Even the ‘conservative’ estimate of a 15% loss of global GDP by 2050 is based on models that account for climate impacts on only 13% of economic sectors and completely ignore tipping-point risks (meaning that actual damage is significantly underestimated) [Planetary Solvency, 2025IFoA & University of Exeter — Planetary Solvency: finding our balance with nature (2025)"the expected value … showing a 15% reduction in global GDP by 2050.""it also excludes 87% of the economy from analysis."PDF · p. 13].

75% of loans to companies in the EU are exposed to risks arising from nature degradation (clean water for production and cooling, pollination for agriculture, and timber for construction) [ECB, 2023]ECB — Surface water scarcity puts ~15% of euro-area output at risk (2025)“72% of euro area firms are critically dependent on ecosystem services … three-quarters of all corporate bank lending”.


Financial-sector blindness

The global economy values natural capital at a massive discount. The financial system continues to direct trillions of dollars into activities that destroy nature, while ignoring the systemic risks this degradation creates for assets.

Since 1992, produced capital per capita has increased by 100%, while natural capital has fallen by 40% [IPBESIPBES Business and Biodiversity Assessment Summary for PolicymakersNatural capital has fallen by 40% since 1992.].


Threat to national security

In 2025, the UK government officially classified global biodiversity loss and ecosystem collapse as a direct threat to national security, capable of leading to food shortages, water crises, forced migration and conflict [HM Government, 2025Global biodiversity loss, ecosystem collapse and national security (2025)“Global ecosystem degradation and collapse threaten UK national security and prosperity.”].

Cascading impacts

Biodiversity loss threatens the provision of ecosystem services on which human societies depend (water, food, clean air). The impacts range from crop failures and epidemics to political instability and the erosion of global prosperity [HM Government, 2025Global biodiversity loss, ecosystem collapse and national security (2025)“Biodiversity loss is putting at risk the ecosystem services on which human societies depend... The impacts will range from crop failures, intensified natural disasters and infectious disease outbreaks to conflict within and between states... Cascading risks result when the impacts of biodiversity loss escalate through a system of connections.”PDF · p. 6]. Forest degradation, for example, will reduce water availability far beyond forest boundaries, intensifying competition for the remaining arable land.

Threat to national security

Ecosystem collapse is highly likely to catalyse a broad range of risks [HM Government, 2025Global biodiversity loss, ecosystem collapse and national security (2025)“Ecosystem collapse is highly likely to drive national security risk... Economic insecurity... Geopolitical competition... Conflict and military escalation... Political polarisation and instability... Migration... Pandemic risk... Non-state actors including terrorist groups will have more opportunities.”PDF · p. 9].
  • Economic instability: Nature is the ultimate asset underpinning the global economy.
  • Geopolitical competition and conflict: Countries and groups will compete for scarce resources — arable land, water, critical minerals and secure transit routes. The likelihood of conflict and military escalation will increase.
  • A catalyst for terrorism: Non-state actors will gain new opportunities amid political instability, acting as mercenaries or pseudo-governments, and may gain control of scarce resources.
  • Erosion of social resilience: Migration will intensify, the risk of new pandemics will increase, and political polarisation and disinformation will grow in vulnerable regions.

Investor takeaway

Biodiversity is foundational infrastructure. Ignoring ecosystem limits causes established business models to suddenly become unviable. The financial sector is largely ‘blind’ to these risks, creating a systemic vulnerability in the valuation of long-term assets.

Chapter

Migration

Climate-related disasters are becoming a powerful driver of internal migration. The economic risks arise not from external ‘waves of refugees’, but from the displacement of millions of people within countries and the loss of labour capacity.


04.10 Migration

Climate migrants: today

In 2025, disasters — storms, floods, fires and droughts — caused 29.9 million new or repeated internal displacements across 140 countries. This was 35% below the record set in 2024, but still 13% above the ten-year average — a year-on-year decline, not a reversal of the trend [IDMC, GRID 2026IDMC — Global Report on Internal Displacement 2026“Disaster displacements declined in 2025 to 29.9 million new or repeated movements across 140 countries and territories. This was a 35 per cent decrease from the exceptionally high levels recorded in 2024 but still 13 per cent higher than the decadal average.”PDF · p. 7].

Two measures need to be distinguished. Displacements (movements) — the number of times people were forced to move during the year; one person may be counted several times in a single year. Internally displaced persons (IDPs) — the number of people still living away from home on a particular date. In 2025, the annual flow of displacements declined, while the cumulative number of people remaining displaced by disasters increased: their consequences persist.

21.6 millionpeople, on average, were displaced by disasters each year in 2012–2021 — the long-term baseline against which the 2025 figure should be viewed [IOM, 2022IOM — Climate Change and Future Human Mobility, Evidence Summary (2022)“In the past decade, an estimated 21.6 million people were internally displaced annually by climate-related hazards worldwide.”PDF · p. 1]

Climate migrants: the future

Estimates of how much the number of climate migrants will increase differ by an order of magnitude. The authors describe the forecasts as ‘indicative at best’ and stress that in some contexts migration may even decline. This is not a reason to ignore the risk — it is a reason not to replace a range with a convenient single figure [JRC, 2025JRC — Forecasting Climate Migration: How Much Do We Really Know? (2025)“Forecasts of the number of climate migrants are indicative at best; the numbers predicted are very much uncertain and some ignore the fact that in some contexts, migration may even decrease.”PDF · p. 2].

The year in these projections is a function of the warming level built into the model, not an independent date. At the current rate of acceleration, the actual timing could move forward by years.

Benchmark estimates of future climate migration

IOM, pessimistic scenario125–216 millioninternal migrants by 2050 due to slow-onset impacts (water stress, crop failures and sea-level rise); 44–113 million under a climate-friendly scenario [IOM, 2022IOM — Climate Change and Future Human Mobility (2022)“Globally, 44–113 million people are projected to internally migrate by 2050 … under a climate-friendly scenario, increasing to 125–216 million people under a pessimistic scenario.”PDF · p. 2]
Range in the literature50–250 million → 0.6–1 billionpeople affected by 2050, rising to 630 million–1 billion by 2100. The upper estimates are an order of magnitude higher than the lower ones [Almulhim et al., 2024npj Climate Action — Climate-induced migration in the Global South (2024)“Estimates suggest that between 50 million and 250 million people could be affected by 2050, rising to 630 to 1000 million by 2100.”PDF · p. 2]
Historical ‘range’150 million–1.4 billionthe range of published estimates for the number of ‘climate migrants’ — research has shifted from early linear models of ‘mass international migration’ towards recognising that movements are predominantly internal and short-distance [JRC, 2025JRC — Forecasting Climate Migration (2025)“The World Bank's Groundswell report projects up to 216 million internal climate migrants across six major regions by 2050.”“…a relative consensus has emerged that environmental changes are most frequently a driver of very short distance movements that are often internal…”PDF · p. 2 (Figure 1)]

The IMF’s conservative estimate and its blind spots

Estimates based only on the observed historical relationship between climate and migration produce cautious figures. An IMF working paper concludes that future flows will rise — from 60 million per decade in 2010 to 88–121 million by 2050 — but that the increase is driven primarily by population growth in origin countries, while changes in average climatic conditions add fewer than 5 million migrants a year [IMF WP, 2024IMF Working Paper WP/24/58 — Climate Variability and Worldwide Migration (Cattaneo et al., 2024)“…the most important driver of migration is population growth, while changes in decadal average climatic conditions alone are responsible for a small fraction of the projected migration flows.”“In most cases, climate change increases the outflows of migrants by much less than 5 million per year.”PDF · pp. 8, 18]. This is a lower bound: the model uses decadal averages, does not account for nonlinear or cascading effects, and its authors themselves acknowledge that under strong warming it moves far beyond the historical sample — meaning that the sensitivity of migration to climate may be underestimated [IMF WP, 2024IMF Working Paper WP/24/58 (Cattaneo et al., 2024)“In other words, for scenarios of very high warming in the far future, we push our model considerably out-of-sample.”“…the role of global warming and intensification of some extreme events appears to be marginal.”PDF · p. 21]. The same methodological trap also understated earlier economic estimates of climate damage — until accounting for cascading effects raised them several-fold.

With that caveat, the model’s own conclusions are:

Calibration

The absolute numbers are disputed and, by the models’ own admission, are probably underestimated. What matters is not so much the volume as the pressure on receiving communities: even relatively small flows already overwhelm cities and exacerbate tensions in destination regions. Climate migration is primarily internal movement within poorer regions, amplified by demographic growth; the focus of risk shifts to the resilience of origin regions, food, water and labour channels, and receiving cities.

The mechanism: how climate drives migration

The link between climate and migration can be traced in data from Mexico: extreme drought during the maize-growing season significantly increases the likelihood of crossing the border illegally the following year. If extreme weather persists at home, migrants are less likely to return — climate does more to keep them abroad than to push new migrants out [Zhu et al., 2024PNAS — Weather deviations linked to undocumented migration and return between Mexico and the United States (Zhu et al., 2024)“Very dry weather has a statistically significant association (P < 0.05) with a higher likelihood of undocumented crossings in subsequent year; other rainfall and temperature extremes do not.”“The weather impacts on migration are small relative to those impacts on return decisions.”PDF · pp. 4, 8].


The paradox: climate both drives people out and ‘traps’ them

The relationship ‘more disasters → more refugees’ is not linear. Climate can lead to both more and less migration — depending on the context and people’s resources. The poorest often cannot leave: migration costs money, and a lack of funds ‘traps’ people in the risk zone.

CLIMATE SHOCK drought · flood · heat PUSH → migration resources available to leave; usually within the country ENTRAPMENT → immobility no means to leave — «trapped populations» REDIRECTION fewer returns → migrants ‘settle’ CITIES pressure on cities
DiagramA climate shock has three outcomes, not one: migration, involuntary immobility and the redirection of flows (usually within the country and to cities). [IMF WP, 2024; JRC, 2025; IOM, 2022]
The burden is asymmetric9 in 10of those potentially affected by environmental change live in low-income countries and small island states — the places that have contributed least to emissions [UNDESA, 2024UNDESA — Climate Change, Forced Migration and Sustainable Urbanization (Trask, 2024)“The majority (nine out of ten) of the people who will be potentially affected by environmental changes are in low-income and small island countries.”PDF · p. 4]

Cities bear the brunt; corridors are reshaped

Because climate migration is predominantly internal, the burden falls not on international borders but on cities — especially the megacities of poorer countries, where infrastructure is already weak. Cities already host 70% of the world’s refugees and displaced people; about 95% of urban growth occurs in low- and middle-income countries [MMC, 2022Mayors Migration Council — Climate Migration in Mexican and Central American Cities (2022)“…the primary destination of international and internal migrants and home to 70 percent of the world's refugees, internally displaced persons (IDPs), and stateless people.”PDF · p. 6].

Climate redistributes people towards major cities within countries and reshapes international corridors — the direction of flows changes as much as their volume.

What this means for business and policy

  • Growing internal displacement, concentrated in East Asia and the Pacific, South Asia and Africa.
  • Transmission of risk through crop yields, water and labour — in other words, into prices and labour supply.
  • ‘Trapped’ groups as focal points of humanitarian and political instability in origin regions.
  • Migration corridors shifting towards Europe and North America.
  • Pre-emptive evacuation as an underestimated but effective form of adaptation.
Investor takeaway

The absolute numbers are disputed and probably underestimated by models, but even moderate flows already create political and fiscal pressure in receiving countries. The planning horizon should be tied to +2 °C and population growth rates in origin countries, not to a single figure.

Chapter

Interconnections


04.11.1

Compound risks: a ‘perfect storm’, climate whiplash and a sequence of shocks

The cumulative effect of several heatwaves and droughts can overwhelm systems that lack sufficient resilience. The main danger is not individual events but their destructive combinations.

Heat and drought dry out the soil Soil — like ‘concrete’ compacts, loses its ability to absorb water More intense downpour +7% moisture per °C — ‘rain bombs’ FLASH FLOOD flash flood — even where none has occurred before
Diagram 5A ‘perfect storm’ of heat and downpours. Projections indicate that by the end of the century, under the >3 °C warming scenario, more than half the world’s population will be exposed to high risk from such compound events every year. [Zhou et al., 2024]

Severe heat and drought dry and compact the soil, turning it into something like asphalt. When a downpour follows, the water does not soak in but runs over the surface, causing catastrophic sudden floods (flash floods) even where none have ever occurred. Warm air holds considerably more moisture (~7% for every degree of warming), so downpours after heat become abnormally intense — ‘rain bombs’. Not only are heatwaves and extreme precipitation becoming more frequent separately, but the likelihood of their dangerous combination is also rising: the atmospheric conditions that produce heat simultaneously ‘charge’ the atmosphere for the powerful downpour that follows [Zhou et al., 2024].


04.11.2 Overlapping shocks

Shocks overlap with the climate crisis

Climate change does not unfold in a vacuum. Wars, supply-chain disruptions and economic shocks that periodically destabilised the world in the past now intersect with the climate crisis. These shocks affect the same vulnerable systems: water supplies, crop yields, food prices and national sovereignty. The combination of conflict and climate shocks is already the leading cause of acute food insecurity worldwide [World Bank, 2026Food and Nutrition Security Update“Conflict and climate shocks continue to be the primary drivers of acute food insecurity ... higher energy, fertilizer, logistics, and food costs are increasing pressure on poorer households”PDF].

Some examples of these interconnections:

Investor takeaway

Compound events and cascading risks change the very nature of how losses arise: they do not add up, they multiply. Models that assess hazards in isolation systematically underestimate the overall risk to regions and portfolios.

Part 5

The financial system's response

Banks · insurers · crisis mechanism · public response · actuaries · a bridge to repricing.

Part 5 · 8 themes

05.1 The banking system's response

Banks acknowledge the 2–3 °C scenario

An analysis of documents from 2024–2025 reveals a fundamental shift in corporate planning: from attempts to prevent climate catastrophe to preparing for its consequences. The findings draw, among other sources, on OMFIF (the independent forum for central banks, sovereign wealth funds and think tanks) and research by the University of Oxford on sustainable finance.

  • From the report BISThe bank for the world's central banks (the bank for the world's central banks), July 2025: ‘regulators are increasingly calling on banks to recognise physical climate risk as a new factor in their risk universe and incorporate it into credit risk management policies. A number of national financial authorities have explicitly set supervisory expectations that banks will adjust their risk management practices in response to climate change’.
  • Morgan Stanley officially stated in March 2025: ‘We now expect a 3 °C world’, citing ‘recent setbacks in global decarbonisation efforts’. This forecast was included in an equity investment report on air-conditioning manufacturers.
  • JPMorgan Chase announced the start of a ‘new climate era’ in early 2025, stating explicitly that ‘climate change is an economic challenge’ and requires climate considerations to be integrated into ‘day-to-day decision-making’. The bank developed its own CAF system to assess clients for climate risks.
  • IIF (an international financial institution representing more than 400 of the world's largest banks) issued a formal statement to the financial sector, putting its position in bold: ‘The world is not on track to limit the temperature rise to below 2 °C’ (February briefing, 2025) [IIF, 2025]IIF — Sustainable Finance Monitor: Can 1.5 Be Kept Alive? (2025)“The world is not on track to limit temperature rise below 2°C – and limiting warming 1.5°C is almost certainly unachievable, without a major step change in policy ambition”PDF · p. 3.
  • NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system (a consortium of the world's central banks, including the ECB and the Federal Reserve) published new official projections in November 2024: under ‘current policies’, the world will reach 2 °C and then 3 °C of warming, while economic damage will be three times higher than previously thought.
In brief

Leading global financial institutions have acknowledged systemic risks and begun formally incorporating global warming scenarios of 2–3 °C into their projections.


Systemic risk: banks are unprepared

The main obstacles are limited risk-modelling capabilities and a lack of data with which to assess these risks.

In brief

Banks recognise the threat but cannot yet measure it accurately. Their models and actions lag behind the pace of change. This means the risks in their loan portfolios are probably substantially underestimated—a colossal hidden risk on bank balance sheets.


What are climate risks?

For banks, climate risk primarily means a deterioration in borrowers' ability to pay. Borrowers face two main types of risk [BIS, Incorporating physical climate risks into banks' credit risk models, 2025]BISThe bank for the world's central banks — Incorporating physical climate risks into banks' credit risk models (2025)“physical risks in banks’ capital requirements, loan loss provisions, pricing of loans … RWA rises as much as by 20%”:

  1. ‘Physical’ risk — damage to assets from natural disasters and extreme weather. This includes the effects of heat on labour, as well as smoke and air pollution (see Part IV).
  2. ‘Transition’ risk — the costs of the shift to the green economy needed to mitigate further impacts: changes in public policy, legislation, regulation and taxation; technological shifts; and changes in market conditions and customer preferences.

05.2 The insurance industry's response

The insurance industry: ‘uninsurable zones’

Banking models show only the ‘tip of the iceberg’. Documents from the world's largest insurers provide a clearer picture of what is happening ‘below the surface’ and why it is potentially catastrophic:

‘We are rapidly approaching temperature levels—1.5 °C, 2 °C, 3 °C—at which insurers will no longer be able to offer cover for many of these risks. The maths does not work: the required premiums exceed what people or companies can afford. This is already happening’

AllianzOne of the world's largest financial services and insurance groups · public statement by a board member, 2025

Investor takeaway

The withdrawal of insurers is the first ‘black swan’ already in flight. Assets in areas the insurance market deems ‘uninsurable’ because the risks are excessively high become ‘toxic’: they lose collateral value and liquidity, and begin generating losses.


Underestimation of physical risks

The problem is compounded by the vast gap between official—and market—risk assessments and assets' actual vulnerability to fires, floods, droughts, hail, hurricanes and mudslides. Official maps, such as those of FEMA, the US Federal Emergency Management Agency, which guide authorities, developers and buyers, are outdated and do not reflect the real risks of a changed climate [Marsh McLennan, 2025Marsh McLennan — 2025 State of Flood Report“increase in flooding events, even in areas previously considered low risk”; FSF, 2025First Street — 8th National Risk Assessment: The Precipitation Problem (2023)“these formerly rare events are now occurring as often as every 5 or 10 years … data that do not reflect current rainfall conditions”].


Public response: migrating towards risk

The situation is further exacerbated because people—and the market—continue to ignore climate risks. Economic development is concentrating in places people need to leave.

  • Homes continue to be built where they should not be, often on a large scale [Swiss Re, 2025].
  • In the United States, migration is not away from risk but directly towards it: people are leaving expensive but safer states such as California and New York and moving in large numbers to the highest-risk states—Florida, Arizona and Texas. Affordable housing and jobs remain the main drivers.
  • Population growth and the concentration of assets continue in the highest-risk areas—from rapid development in hurricane-prone Florida to urban growth in regions exposed to severe convective storms [Aon, Climate and Catastrophe Insight, 2025].

This trend does more than increase the number of future victims: it systematically concentrates future financial losses and ‘hidden credit risks’ in geographic danger zones [FSF, 2025; Aon, 2025].

Investor takeaway

Climate change could substantially deepen economic inequality, turning it into a geographic divide: affluent groups will be able to buy safety in expensive ‘climate havens’, while the economically vulnerable will be trapped with depreciating assets and growing threats.


Uninsured risk: a $1.8 trillion ‘protection gap’

$1.8 trillion‘protection gap’—the record gap between total damage and insured losses (2022)[UNU-EHS, 2023]
~25%the share of economic losses from climate disasters that is insured in Europe[EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)]
60%of all losses in Europe were uninsured in 2024[Aon, 2025]
94% / 93%insurance protection gap in China and India: almost all losses are uninsured[Allianz, 2025]

The $1.8 trillion ‘protection gap’ is effectively the ‘dark matter’ of the financial system: risk that is neither recognised, assessed nor managed, creating enormous systemic vulnerability [UNU-EHS, 2023]. Emerging economies have vast protection gaps (China 94%, India 93%, South Africa 83%), while the gaps are smaller in advanced economies (UK ~21%, Australia ~30%, Canada ~35%) [Allianz Research, Climate Adaptation Report, 2025]. In Greece, the gap exceeds 80%—only 18.2% of homes are insured [WWA, 2025World Weather Attribution (2025)“In March 2025, only 18.2% of residences were insured”PDF · p. 31]. The case of Italy: an 83% gap, 75% of homes in risk zones, and 98% of seismic losses in 1980–2021 uninsured.


Systemic risk: insurers are unprepared

Part 6 · breaking point

Financial crisis

The withdrawal of insurers from entire regions sets off a chain reaction across the financial system—from mortgage markets to sovereign debt.

Part 6 · turning point

06.1 Insurer's warning · AllianzOne of the world's largest financial services and insurance groups, 2025

A board member of AllianzOne of the world's largest financial services and insurance groups, one of the world's largest insurers, explicitly warns of a potential cascading financial crisis that starts with the withdrawal of insurers and leads to a collapse in the mortgage market and banking instability:

‘This is not a one-off market adjustment. This is a systemic risk that threatens the very foundation of the financial sector. If insurance becomes unavailable, other financial services become unavailable too. A home that cannot be insured cannot be mortgaged. No bank will lend against a property that cannot be insured. Credit markets freeze. This is a credit crunch caused by climate change.

This applies not only to housing, but also to infrastructure, transport, agriculture and industry. The economic value of entire regions—coastal, arid and wildfire-prone—will begin to disappear from financial balance sheets. Markets will reprice these assets rapidly and harshly. This is what climate-driven market failure looks like.’

Günther Thallinger · board member of AllianzOne of the world's largest financial services and insurance groups, 2025

Read the full statement Full text of the post ‘Climate, risk, insurance: the future of capitalism’. The two passages quoted above are italicised. Expand

Climate, risk, insurance: the future of capitalism

Carbon dioxide emissions directly increase the amount of energy retained in the Earth's atmosphere. This is neither a vague nor a future problem—it is physical reality. The more emissions, the more energy is retained. The more energy, the more extreme the atmosphere's behaviour. Storms intensify. Heatwaves last longer. Rainfall becomes heavier. Droughts deepen. This is the starting principle.

These extreme weather events create direct physical risks for every category of asset people own: land, homes, roads, power lines, railways, ports and factories. Heat and water destroy capital. Flooded homes lose value. Overheated cities become uninhabitable. Entire asset classes are deteriorating in real time, resulting in lost value, business disruption and system-wide market depreciation.

The insurance industry has historically managed these risks. But we are rapidly approaching levels of warming—1.5 °C, 2 °C, 3 °C—at which insurers will no longer be able to offer cover for many of them. The maths ceases to work: the required insurance premiums exceed what people or companies can pay. This is already happening. Entire regions are becoming uninsurable. See: the 2023 withdrawal of State Farm and Allstate from California's home-insurance market because of wildfire risk.

This is not a one-off market adjustment. This is a systemic risk that threatens the very foundation of the financial sector. If insurance is no longer available, other financial services become unavailable too. A home that cannot be insured cannot be mortgaged. No bank will lend against an uninsurable property. Credit markets freeze. This is a climate-driven credit crunch.

This applies not only to housing, but also to infrastructure, transport, agriculture and industry. The economic value of entire regions—coastal, arid and wildfire-prone—will begin to disappear from financial balance sheets. Markets will reprice them rapidly and ruthlessly. This is what climate-driven market failure looks like.

Some argue that the state will step in where insurers withdraw. But this assumes that the state—that is, the taxpayer—can afford to do so. That assumption is already breaking down. Covering the cost of three or four major wildfires or floods in a single year strains public budgets to the limit. If several costly events occur in quick succession, as climate projections indicate, no government can realistically cover the damage without severe austerity or collapse. See: Germany's 2021 flood relief of €30 billion; the increase in Australian disaster-relief spending in 2020–2023.

There is also false comfort in ‘adaptation’, because many risks allow no meaningful adaptation. It is impossible to ‘adapt’ to temperatures beyond the limits of human endurance. The scope for adapting to megafires is limited; in practice, the only option is not to build near forests. Entire cities built on floodplains cannot simply move uphill. And as temperatures continue to rise, adaptation itself becomes economically unviable.

Once warming reaches +3 °C+3,8 °C, the situation becomes locked in. Atmospheric energy at that level will persist for more than 100 years because of the inertia of the carbon cycle and the absence of scalable industrial carbon-removal technologies. There is no known pathway back to conditions below 2 °C. See: IPCC Sixth Assessment Report, 2023; NASA Earth Observatory, ‘The Long-Term Warming Commitment’.

At that point, risk cannot be transferred because there is no insurance. It cannot be absorbed because governments lack the capacity. Adaptation cannot address it because physical limits have been exceeded. This means no more mortgage lending, no new development, no long-term investment and no financial stability. The financial sector as we know it ceases to function. And with it, capitalism as we know it ceases to be viable.

Capitalism must now address this existential threat. The idea that market economies can continue to function without insurance, finance and asset protection is a fantasy. There is no capitalism without functioning financial services. And there are no financial services without the ability to assess and manage climate risk.

There is only one path forward: prevent any further increase in the level of energy in the atmosphere. That means preventing emissions from entering the atmosphere. It means burning less carbon-based fuel or capturing emissions at the point of combustion. These are the only two levers. Everything else is delay or distraction.

The good news is that we already have the technologies to move from burning fossil fuels to zero-emission energy. Solar power, wind power, battery energy storage, green hydrogen, electrification, grid upgrades and demand-side efficiency are all mature, scalable solutions.

All that is missing is speed and scale—and an understanding that this is not about saving the planet. It is about preserving the conditions in which markets, finance and civilisation itself can continue to function.

Source: Günther Thallinger, LinkedIn, 2025 — «Climate, risk, insurance: the future of capitalism».

06.2 Crisis mechanism

Crisis mechanism: a 5-step chain

BISThe bank for the world's central banks, the UN, EEAEuropean Environment Agency and AllianzOne of the world's largest financial services and insurance groups confirm that, over the past few years, physical risks have moved from a niche concern for insurers to a systemic risk factor for financial markets. The collapse of insurance is a direct mechanism leading to a financial crisis [UNU-EHS, 2023UNU-EHS — An uninsurable future? The insurance protection gap and climate change (2023); BIS, 2025BIS — Incorporating physical climate risks into banks' credit risk models (2025)“Climate change presents a systemic risk”; EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)“from a niche domain of (re)insurers into a systemic risk factor”].

Insurance withdrawal
CauseClimate risks become unpredictable or excessively high.Consequence‘Uninsurable zones’ emerge, where insurance is either unavailable or prohibitively expensive.
Asset-market collapse
CauseBanks stop lending to finance purchases of assets in ‘uninsurable zones’ or accepting those assets as collateral.ConsequenceThe property market freezes and asset values fall sharply because of illiquidity and direct risk.
Banking crisis
CauseAssets on bank balance sheets that are concentrated in affected regions and serve as collateral for existing loans lose value.ConsequenceBanks incur direct losses from widespread arrears and defaults by borrowers who lose their ability to pay after another disaster.
Sovereign debt crisis
CauseThe state is forced to cover uninsured losses and recapitalise banks—while disasters become more frequent and severe, food prices rise, infrastructure deteriorates and people's capacity to work declines.ConsequenceA sharp rise in public debt and a loss of investor confidence trigger a debt crisis.
A negative spiral begins
CauseFinancial buffers are depleted; recovery from each new disaster becomes slower and more expensive.ConsequenceThe system loses stability and its capacity to recover—leading to chronic economic decline and social destabilisation.

The parallel with 2008 and capital requirements

Physical climate risks reach a bank's balance sheet and income statement through several channels: disasters incapacitate borrowers' assets, reducing collateral values and income from damaged properties; because climate events affect many borrowers simultaneously, increasing default correlation, a bank with lending concentrated in a risk zone can suffer substantial losses (making regional banks particularly vulnerable) [BIS, 2025BIS — Incorporating physical climate risks into banks’ credit risk models (2025)“Physical risks are transmitted to a bank’s balance sheet and P&L through different channels. For example, natural disasters... affect households and corporate borrowers by impairing their fixed assets... This, in turn, impacts the creditworthiness of the obligors by decreasing the value of collateral...”“Since climate-driven events commonly affect multiple borrowers at the same time, thus driving up correlation of defaults in the loan portfolio, a bank may incur in significant losses if it has a concentration of credit exposures...”PDF].

This resembles the 2008 crisis, but the root cause is not a temporary problem with toxic securities; it is the permanent physical vulnerability of assets that are gradually dropping out of the economy. This is why BISThe bank for the world's central banks and the ECB propose integrating climate risks into prudential rules—that is, increasing banks' capital requirements (RWA) [BIS, 2025BIS — Incorporating physical climate risks into banks’ credit risk models (2025)“...standard setting bodies and financial regulators have increasingly urged banks to recognise physical climate risk as a new factor in their risk space and internalise it in their credit risk management policies.”“...account for physical risks in banks' capital requirements, loan loss provisions...”“...Model RWA, when physical risk-related corrections are included, increases by around 7.9% [up to 20%] compared to the original calculations...”PDF]. This directly hits banking-sector profitability, forcing banks either to raise interest rates or reduce lending.


Quantifying the risk to banks:

  1. Historical data: every 1% increase in insurance premiums causes the mortgage default rate to rise by 1.05 percentage points [FSF, The 13th National Risk Assessment, 2025First Street — 13th National Risk Assessment: Climate, the 6th C of Credit (2025)“Every 1 percent-point increase … 1.05 percentage-point rise in foreclosure rates”].
  2. Historical data: for the most vulnerable group—damaged homes in river flood zones—the number of mortgage defaults rises by 62.8% compared with the pre-flood period [FSF, 2025First Street — 13th National Risk Assessment: Climate, the 6th C of Credit (2025)“properties saw a 62.8% increase … Riverine (Fluvial)”; Aon, 2025].
  3. Nature degradation: 75% of loans to EU companies are exposed to risks from nature degradation (clean water for production and for cooling factories and data centres, pollination for agriculture, and timber for construction) [ECB, 2023]ECB — Surface water scarcity puts ~15% of euro-area output at risk (2025)“72% of euro area firms are critically dependent on ecosystem services … three-quarters of all corporate bank lending”.
  4. FSF projection model: over the next 10 years, banks' annual losses from climate-related defaults will increase more than 4-fold (from $1.2 billion to $5.4 billion), accounting for almost 30% of all mortgage credit losses [FSF, 2025First Street — 13th National Risk Assessment: Climate, the 6th C of Credit (2025)“$1.21 billion in bank losses in 2025 … rise credit losses to $5.36 billion”].
  5. Projection model of BISThe bank for the world's central banks (a loan secured on commercial property in Alabama, using the current probability of a severe hurricane in 2025): probability of default increased by 12%; loss given default rose from 10% to 24.8%; required capital increased by 8%, 15.5% and 22%, depending on the scenario [BIS, 2025].

Consequences for ‘uninsurable zones’

‘Uninsurable zones’ are not merely a problem for homeowners. They trigger a freeze in mortgage lending, rising credit risks for the banking system and the long-term economic decline of entire regions. These cascading, systemic effects are generally excluded from standard risk-assessment models.

Regional economic decline: affluent households and businesses leave ‘uninsurable’ zones; the cost of capital rises, investment falls and the tax base shrinks; disasters recur without the resources needed for recovery, turning regions into depressed, subsidy-dependent areas that drain the state's overall budget.

Growing social inequality: the most vulnerable groups cannot leave and remain in deteriorating, increasingly dangerous areas; the loss of insurance and growing number of disasters exacerbate stress and mental-health problems.

06.3 · Systemic risk The state as the backstop

The state as the backstop

Some argue that the state will step in where insurers withdraw. But this assumes that the state—that is, the taxpayer—can afford to do so. That assumption is already breaking down. Covering the cost of three or four major wildfires or floods in a single year pushes public budgets to the limit. If several costly events occur in quick succession—as climate projections indicate—no government can realistically cover the damage without severe austerity or collapse. Examples include Germany's €30 billion in relief for flood victims in 2021 and Australia's rising disaster-response costs in 2020–2023.

Günther Thallinger · board member of AllianzOne of the world's largest financial services and insurance groups, 2025

To put the scale in perspective

From ‘individual disasters’ to ‘permanent crisis’

Hurricane Helene struck Florida's Big Bend region in autumn 2024, becoming the strongest hurricane in the region's history. 13 days later, Hurricane Milton hit Florida, becoming one of the most intense Atlantic hurricanes. This set a record for the shortest interval between major hurricanes in Florida. Combined damage was about $113 billion [NOAA, 2025NOAA — Hurricane Costs“strongest hurricane on record to strike the Big Bend region of Florida”“Helene’s total costs were $78.7 billion.”“Total costs for Milton were $34.3 billion.”; NHC, 2025NHC — Hurricane Milton Tropical Cyclone Report“one of the strongest hurricanes of record in the Atlantic basin”“This ties Hurricane Rita of 2005 for the fourth-lowest minimum central pressure in an Atlantic hurricane.”; Moody's RMS, 2024Moody's RMS — Hurricane Milton: Live blog“Milton made landfall 13 days after Helene”“the fewest number of days between major hurricane landfalls in Florida on record”]. Three months later, the Los Angeles fire added another $65 billion to total US losses, making it the costliest fire to date [Bloomberg, 2025Bloomberg — The Climate Economy 2025 Outlook“Los Angeles wildfires in January 2025 causing $65 billion in economic costs”; Munich Re, 2026Munich Re — Wildfires and bushfires“The costliest wildfires to date ... struck the Los Angeles area in January 2025”].

06.4 Systemic risk

Climate is the world's No. 1 threat

The World Economic Forum (WEF) report «The Global Risks Report 2026» puts the global expert view into perspective.

Long-term threat: Over a 10-year horizon, the top three positions in the ranking of the most severe global risks (by impact) are occupied exclusively by environmental threats. Their potential damage is rated more highly than that of AI or geoeconomic confrontation [WEF, 2026World Economic Forum — The Global Risks Report 2026Top 3 severe risks over 10 years: 1. Extreme weather events. 2. Biodiversity loss and ecosystem collapse. 3. Critical change to Earth systems.PDF · p. 9]:

  • 1st place. Extreme weather events.
  • 2nd place. Biodiversity loss and ecosystem collapse.
  • 3rd place. Critical changes to Earth systems (‘tipping points’ or ‘points of no return’).

Short-term threat: Even over a 2-year horizon, extreme weather events firmly occupy fourth place among threats to the world.

Climate change remains the leading overall risk for both experts and the general public [AXA, Future Risks Report, 2025]AXA — Future Risks Report 2025“Climate change remains the top risk overall for both experts and the general population.”.

Investor takeaway

The view that climate change is the foremost global threat over the next decade is a consensus among the world's experts. It is no longer a marginal view.


06.5 Underestimation of systemic risk

Underestimation of systemic risk

Regulators, central banks and the largest insurers have independently reached the same conclusion: climate change is a systemic risk to the entire financial system.

Investor takeaway

Systemic climate risk is acknowledged at the highest level but remains underestimated in models and prices. An environment of fragmentation and ‘polycrisis’ only magnifies it.

06.6 Supply chains

Supply chains: diversification is no panacea

A working paper by BISThe bank for the world's central banks quantifies the ‘domino effect’ in the real economy, showing that climate risk is not a local problem but a networked virus spreading through the arteries of the global economy. A climate shock, such as a drought, in one region causes GDP to fall in another geographically distant region if the two have trade links. Municipalities whose customers are affected by drought experience GDP growth declines of 1–2 percentage points [BIS, Supply chain transmission of climate-related physical risks, 2025].

  • Impacts are felt everywhere: the cascading effect leads to lower imports and worse labour-market outcomes—higher unemployment and lower wages—in regions not directly affected by the disaster.
  • Even ‘moderate’ shocks are dangerous: most damage is transmitted through supply chains not by rare megadisasters, but by moderate, more frequent anomalies such as a ‘minor’ drought. The risk is persistent, not episodic.
  • Sector vulnerability: agriculture is vulnerable to both local and distant shocks; industry is more resilient to moderate shocks but suffers severely from intense disasters affecting suppliers; the service sector is affected mainly by local shocks.

NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system models probable damage in the coming years: global GDP falls by as much as 1.0% in 2026 following extreme events in Europe and by up to 2.1% in 2027 following events in Asia. In some scenarios, persistent GDP losses reach 2.8% and unemployment rises by up to 1.7 percentage points in 2028. Supply-chain ‘bottlenecks’ can cause global GDP losses of more than 3%, while regional losses peak at 12.5% of GDP in Africa [NGFS, Short-Term Scenarios, 2025].

Investor takeaway

The effectiveness of geographic diversification is declining rapidly: an industrial company in a prosperous region is vulnerable to a drought thousands of kilometres away if it sources key components from, or sells its products to, that location.

Chapter

Actuarial assessment

‘Planetary solvency’: the resilience of the economy and financial system is assessed in the same way as an insurer's solvency—against rare catastrophes (the ‘tails’), not the average projection.

06.6.1 An actuarial perspective

Climate as a solvency issue

Actuaries are financial analysts who calculate the risk of rare but devastating events for insurers and pension funds. They have applied this approach to climate and nature: the system must withstand not the average scenario, but its ‘tail’—a low-probability catastrophe.

Actuaries call the worst such outcome ‘ruin’ —the loss of prosperity through severe socio-economic destruction. Under current policies, they assess its risk as ‘non-negligible’: unacceptably high to ignore [Planetary Solvency, 2025IFoA & University of Exeter — Planetary Solvency: finding our balance with nature (2025)"…the scale and pace of human activity has continued to drive planetary outcomes, with a non-trivial risk of ruin — the loss of prosperity due to severe societal and economic disruption."PDF · p. 8]. In quantitative terms, ‘catastrophic-to-extreme’ impacts are already considered likely by 2050 [Planetary Solvency, 2025IFoA & University of Exeter — Planetary Solvency: finding our balance with nature (2025)"the trajectory is concerning, with Catastrophic to Extreme impacts Likely or Highly Likely by 2050."PDF · p. 27], but accelerating warming could bring that point forward significantly.



The urgent need for risk management

‘We use the example of climate risk assessment to show why and how decision-makers may inadvertently have accepted much higher levels of risk than they assume’ [Planetary Solvency, 2025IFoA & University of Exeter — Planetary Solvency: finding our balance with nature (2025)"We use the case study of climate change risk assessments to highlight why and how policymakers may have inadvertently accepted much higher levels of risk than they think."PDF · p. 10].

The target «net zero 2050» scenario provides only a 50% chance of keeping warming below 2 °C. This scenario is the main climate target for most governments and many companies worldwide: it assumes that global CO₂ emissions reach net zero by 2050. [NGFS Scenarios PortalNetwork for Greening the Financial System — NGFS Scenarios Portal"Net Zero 2050 limits global warming to 1.5°C through stringent climate policies and innovation, reaching global net zero CO2 emissions around 2050."NGFS Scenarios Portal · Net Zero 2050 scenario; Climate Action TrackerClimate Action Tracker — CAT net zero target evaluations"around 145 countries had announced or are considering net zero targets""The countries cover close to 77% of global emissions."Climate Action Tracker · 2025; SBTi Corporate Net-Zero StandardScience Based Targets initiative — Corporate Net-Zero Standard"provides companies with the guidance and tools needed to set science-based targets aligned with reaching net-zero emissions by 2050 at the latest."SBTi · Corporate Net-Zero Standard].

Actuaries point to a logical inconsistency: society and business accept an enormous 50% risk of global climate ruin, while, by comparison, the legally permitted risk of an insurer becoming insolvent is just 0.5% [Planetary Solvency, 2025IFoA & University of Exeter — Planetary Solvency: finding our balance with nature (2025)"This probability of failure is very high when compared to … society's appetite for insurance company failure, which is set at 0.5%, a one in 200 year chance."PDF · p. 22].

Moreover, the world is not yet following even this pathway. If current trends continue, warming could reach 2.5–3 °C or more [NGFS Scenarios PortalNetwork for Greening the Financial System — NGFS Scenarios Portal"Under the NGFS Current Policies Scenario, global warming of 1.5 °C could be reached in the 2030s, 2 °C around 2050 and 3 °C around 2100.""If no further measures are introduced, 3 °C or more of warming could occur by 2100."NGFS Scenarios Portal · Current Policies scenario]. Yet such projections are based on average estimates, while an overlooked extreme-warming scenario of 4.5 °C or more has an 18% probability.

06.6.2 Climate tail risks

Damage to GDP rises non-linearly

Between +1,5 °C and +2 °C climate damage begins to exceed total annual global GDP growth (about 3% per year) [Parasol Lost, 2026IFoA & University of Exeter — Parasol Lost: Recovery plan needed (2026)"climate damages increasing rapidly above 1.5°C of warming and overwhelming the global GDP growth rate of 3% per annum, between that temperature and 2°C of warming."PDF · p. 20]. Beyond that, losses accelerate: about 30% of GDP at +3 °C and up to 80% at +4 °C [Climate Scorpion, 2024IFoA & University of Exeter — Climate Scorpion: the sting is in the tail (2024)"around 30% GDP loss occurs at 3°C of warming, compared with 80% GDP loss using the 4°C ruin parameterisation.""this is purely an illustrative example."PDF · p. 28]. These mathematical damage models are intended to illustrate the dynamics of rapidly compounding losses, not to provide a precise economic forecast.

06.6.3 Breaching planetary boundaries

7 of 9 boundaries breached—the risk is irreversible

‘Planetary boundaries’ are safe limits for nine Earth systems, including climate, freshwater and biosphere integrity. By 2025, 7 of the 9 had been breached, compared with 6 in 2023 [Tipping into the wild unknown, 2026IFoA & Anglia Ruskin University — Planetary Solvency: Tipping into the wild unknown (2026)"9 boundaries assessed / 7 crossed"PDF · p. 10 (Figure 1)]. The key difference from ordinary risk is that recovery beyond a tipping point cannot be assumed: this is ‘not a risk of volatility, but of irreversibility’ [Tipping into the wild unknown, 2026IFoA & Anglia Ruskin University — Planetary Solvency: Tipping into the wild unknown (2026)"Beyond a tipping point, recovery cannot be assumed to be possible … The risk is not just volatility, it is irreversibility."PDF · p. 9]. Breaching these limits deprives humanity of a safe operating space and sharply increases the risk of sudden ecosystem collapse [HM Government, 2025Global biodiversity loss, ecosystem collapse and national security (2025)“As of 2023, six boundaries have been crossed: (1) biosphere integrity... (6) novel entities...”PDF · p. 6]. Many of nature's services are irreplaceable: they cannot simply be ‘bought back’ [Planetary Solvency, 2025IFoA & University of Exeter — Planetary Solvency: finding our balance with nature (2025)"Ecosystem services are often non-substitutable … their loss undermines economic production."PDF · p. 11].

9 boundaries assessed in total 3 / 7 4 / 7 6 / 9 7 / 9 2009 2015 2023 2025
The number of breached planetary boundaries is rising. [Tipping into the wild unknown, 2026IFoA & Anglia Ruskin University — Planetary Solvency: Tipping into the wild unknown (2026)"2009 … 7 boundaries assessed 3 crossed … 2025 … 9 boundaries assessed 7 crossed"PDF · p. 10 (Figure 1)]

Projection if current trends continue

Each risk is plotted on two axes—‘how severe’ (from ‘limited’ to ‘extreme’) and ‘how likely’—showing its position in 2025 and trajectory towards 2050.

Extreme ≥3 °C by 2050 Catastrophe ≥2 °C by 2050 Decimation up to 2 °C by 2050 Severe 1.5 °C (overshoot) Limited <1.5 °C by 2050 Extremely unlikely Very unlikely Unlikely Possible Likely Very likely 40–60% 60–90% ≥90% Society 2025 Nature 2025 Climate 2025 Economy 2025 Climate 2050 Nature 2050 Society 2050 Economy 2050 2025—current position 2050—trajectory Climate · by 2050Trajectory from ‘catastrophe’ (≥2 °C by 2050, a partial cascade of tipping points) to ‘extreme’ (≥3 °C by 2050, multiple tipping points and a full cascade). Nature · by 2050From ‘catastrophe’ (breakdown of some critical ecosystems and Earth systems, mass extinctions and severely disrupted ocean circulation) to ‘extreme’ (breakdown of a number of critical ecosystem services and high levels of extinction among higher forms of life). Society · by 2050‘Decimation’ level: severe socio-political fragmentation in regions affected by climate and nature; collapse of vulnerable states and mass casualties in affected areas. Economy · by 2050From ‘severe’ (GDP loss ≥5% / >$5 trillion per year; mortality ≥5% / >400 million) to ‘decimation’ (GDP loss ≥10% / >$10 trillion per year; mortality ≥10% / >800 million). Society · now (2025)‘limited’ → ‘severe’. Several centres of geopolitical tension and active conflicts with the risk of spreading; fragile states vulnerable to climate and nature; growing economic protectionism. Nature · now (2025)Trending towards ‘severe’. Stress on water and food systems is increasing; natural assets continue to degrade, several planetary boundaries have been breached and extinction rates are high; agreements exist, but implementation is weak. Climate · now (2025)‘Severe’ level. The number of events causing losses of $1 billion or more and episodes causing 10,000 or more deaths worldwide is rising; greenhouse-gas emissions and concentrations continue to increase; the energy transition is accelerating. Economy · now (2025)‘Limited’ level. Economic damage remains limited for now, but the scale of climate events and associated losses continues to grow.
‘Planetary Solvency’ dashboard: 2025 position (outline) and trajectory towards 2050 (fill) across four dimensions. Below each severity level is the climate threshold; probability thresholds and level definitions are from the «Risk impact matrix», p. 32. Hover over a label: for 2025, it shows the current situation in that dimension; for 2050, the trajectory (levels from the «Risk impact matrix», p. 32). [Global Tipping Points: Planetary SolvencyGlobal Tipping Points — Planetary Solvency Dashboardglobal-tipping-points.org]

Where we are in 2025. The risk position rose sharply over the year and moved beyond acceptable levels. Climate is at the ‘severe’ level; nature is expected to reach ‘severe’ in the near term. Social fragmentation is growing, with active conflicts, geopolitical tension and pressure on vulnerable states. Economic losses and mortality remain ‘limited’ for now.

Where we are heading. The trajectory pushes every risk further beyond acceptable levels; breaches of risk tolerance are likely. Immediate policy action is needed to reduce the risk of ‘catastrophic’ impacts or worse—within this century and possibly well before 2050 [Global Tipping Points: Planetary SolvencyGlobal Tipping Points — Planetary Solvency Dashboardglobal-tipping-points.org].

By dimension: current position and trend towards 2050 [Global Tipping Points: Planetary SolvencyGlobal Tipping Points — Planetary Solvency Dashboardglobal-tipping-points.org]

1 · Climate   now: high trend: critical

  • 2025: Already at the ‘severe’ level: the number of events causing losses of >$1 billion and episodes causing 10,000 or more deaths is rising; emissions continue to increase.
  • 2050: Beyond 1.5 °C, tipping points increase risk exponentially. Current emissions indicate warming of >2 °C by 2050—the ‘catastrophic’ level is very likely (≥90%), while ‘extreme’ is possible (40–60%).

2 · Nature   now: high trend: critical

  • 2025: From ‘limited’ to ‘severe’: several planetary boundaries have been breached, the extinction rate is high, and stress on water and food systems is increasing.
  • 2050: Interconnected risks increase the threat of ecosystem collapse. ‘Catastrophic’ impacts are very likely (≥90%), while ‘extreme’ impacts are possible (40–60%).

3 · Society   now: moderate trend: high

  • 2025: From ‘limited’ to ‘severe’, at times reaching ‘decimation’ in vulnerable states; numerous active conflicts and growing protectionism.
  • 2050: Water, food and heat stress intensify migration and conflict. Impacts ranging from ‘severe’ to ‘decimation’ have a ‘possible’ to ‘likely’ probability (40–90%).

4 · Economy   now: low trend: high

  • 2025: The impact remains ‘limited’ for now, although the scale of climate events and losses is rising towards 1% of GDP.
  • 2050: Damage equal to 19% of GDP by 2050 (that is, a significant slowdown in growth). However, this figure excludes tipping points and many other risks. Given the high uncertainty and interconnected risk factors, a ‘decimation’ or ‘catastrophe’ level is possible (40–60% probability;>25% loss of GDP).
Investor takeaway

Climate and nature are no longer a distant scenario but a tail risk now materialising, which actuaries assess as a non-negligible risk of ‘ruin’—a breach of solvency limits. Warming is at the threshold of 1.5 °C and accelerating; the loss of the aerosol ‘umbrella’ could sharply accelerate it, while tipping points already crossed—reefs, soils and forests—are irreversible. Financial models that assume mean reversion after a shock understate this risk; at the macroeconomic level, its scale is comparable to a systemic financial crisis within the coming decade.

Chapter

Adaptation

Reducing losses requires vast investment in physical protection and infrastructure adaptation. Yet the world is ‘running out of resources’: it is preparing for climate change but lacks the means to achieve resilience [UNEP AGR, 2025UNEP — Adaptation Gap Report 2025 (2025)“Action on adaptation is still inadequate.”PDF · p. 1].

Insufficient measures

The current pathway, based on legislation already enacted, is leading the world towards warming of +3 °C+3,8 °C [NGFS, Phase V, 2024]NGFSA group of central banks and supervisors, including the ECB and the Federal Reserve, established to help green the financial system — Climate Scenarios for central banks and supervisors, Phase V (2024)“Current Policies assumes that only currently implemented policies are preserved, leading to high physical risks”“Current Policies 3.0 °C”. This is a dual systemic failure: a lack of political will to mitigate warming by reducing GHG emissions, and a vast funding shortfall for adaptation—protection against climate risks already embedded in the system.


GHG emissions are rising, while finance flows into hydrocarbons

Despite political declarations, a structural energy transition is not yet under way. Data from the 2025 Lancet Countdown report reveal a paradox: amid record climate threats, the global community continues to invest in the factors causing those threats.

Meanwhile, humanity is missing the enormous health benefits of decarbonisation: phasing out coal could prevent 1 million deaths every year [Lancet Countdown, 2025The 2025 report of the Lancet Countdown on health and climate change“1·00 million annual deaths were still attributable to coal combustion globally in 2022”PDF · p. 26].


Adaptation, by contrast, is critically underfunded

Adaptation is not optional but a condition for survival, yet global investment in it is grossly inadequate [Allianz, Research Climate Adaptation Report, 2025Allianz — Rethinking climate adaptation for global resilience (2025)“adaptation finance remains severely underfunded … Adaptation is no longer an option; it is a survival”].

Even wealthy countries can no longer adapt their own infrastructure fast enough: climate risks are growing faster than budgets, projects and governance systems.

In the UK, the official independent body established by law to assess climate policy and report to Parliament judged the country's preparedness for climate risks in 2025 to be inadequate: it found not a single area of adaptation delivery that could be rated ‘good’. [CCCClimate Change Committee — About“The Climate Change Committee (CCC) is an independent, statutory body established under the Climate Change Act 2008.”“...to report to Parliament on progress made in... preparing for and adapting to the impacts of climate change.”Official website; CCC, 2025Progress in adapting to climate change: 2025 report to Parliament“The UK’s preparations for climate change are inadequate.”“In terms of adaptation delivery, we do not find evidence to score a single outcome as ‘good’.”PDF · 2025 report to Parliament].

New York already faces growing risks from heat, coastal storms and extreme rainfall. About 2.5 million residents live in the 100-year floodplain. The FiDi-Seaport protection project alone is estimated to cost $5.5 billion in 2025 prices; if construction begins in 2029, its cost could rise to $8–9 billion. The city explicitly states that no single source of funding is sufficient for a project of this scale [NYC ComptrollerNYC Climate Dashboard — Resiliency“Today, nearly 2.5 million New Yorkers live in the 100-year floodplain.”Website; FiDi-Seaport Climate Resilience PlanImplementation — Project Cost“The estimated capital cost ... is $5.5 billion in 2025 dollars.”“...with escalation, the total project cost will be an estimated $8-9 billion.”“no single funding stream would be sufficient”Website · Implementation].


Developing countries: adaptation needs are many times greater than actual finance

Adaptation action ‘remains inadequate’, while the finance needed for it is ‘woefully inadequate’ [UNEP AGR, 2025UNEP — Adaptation Gap Report 2025 (2025)“Action on adaptation is still inadequate.”PDF · p. 4; UNEP AGR, 2025UNEP — Adaptation Gap Report 2025 (2025)“the financial resources needed to enable adaptation action in developing countries at the scale necessary to meet the growing challenges of current and future climate risks is woefully inadequate.”PDF · p. 10]. The gap between needs and actual finance is not narrowing [UNEP AGR, 2025UNEP — Adaptation Gap Report 2025: Running on empty (2025)“The adaptation finance gap is not reducing, and the Glasgow Climate Pact goal will be missed under current trajectories.”PDF · p. 7].

Investor takeaway

The global economy is critically unprepared for climate impacts that are already locked in. This vast adaptation deficit creates colossal systemic risk.


Additional barriers to adaptation

Beyond the financing gap, the implementation of adaptation measures faces a number of systemic constraints:

  • Lack of time and slow institutional cycles: Many government strategies are designed around 2050 and 2100 horizons, yet the pace of climate change regularly exceeds conservative projections. Meanwhile, designing, financing and building major protective infrastructure takes years or decades. Today's institutional cycles are too slow to respond in time.
  • Ignoring tail risks: Most baseline models and strategies, including Net Zero scenarios, focus on the most likely outcomes and exclude cascading or tail risks (see ‘Actuarial assessment’). Planning therefore makes no allowance for extreme deviations for which the global economy may be unprepared.
  • Global competition for resources: A mass shift towards adaptation could begin all at once—for example, after a major climate catastrophe that fundamentally changes society's assessment of risk. A sharp global surge in demand for adaptation projects could intensify competition for finance, construction capacity, materials and specialist expertise.

Key causes of ineffectiveness

  • Short-term thinking: Political and financial systems are geared towards short electoral cycles and quarterly reporting, while climate risks are wrongly perceived as a problem for the distant future (2050–2100).
  • Discounting the future: Under current economic models, future losses are discounted. In the short term, cheap fossil fuels deliver greater financial and political benefits than a capital-intensive energy transition and preventive adaptation.
  • Lack of enforcement mechanisms: The global nature of the problem requires collective action, yet there are no effective institutional mechanisms at international level for monitoring and strictly enforcing climate commitments.
  • Underestimation of risks: The full picture of the problem—its interconnections, systemic nature and the severity of its irreversible consequences—remains poorly understood.

Historically, social mobilisation on this scale occurs in response to an obvious and immediate threat to survival. Yet the nature of climate change means that the level of danger and the scale of the threat will probably be felt and widely recognised much later.


Part 7

The Coming Repricing

Inevitable, sudden and two-sided · real estate · mispricing the world’s largest asset class · ‘Minsky moment’ · modelling BISThe bank for the world's central banks

Part 7

07.1 Inevitable · sudden · two-sided

The Coming Repricing

Markets currently ignore physical risks, creating a ‘climate bubble’ in asset prices. A correction is inevitable and is unlikely to be smooth.

  1. Why is repricing inevitable? Regulators (BISThe bank for the world's central banks, the ECB), auditors (Big 4) and reporting standards (IFRS) already require banks and companies to quantify and disclose climate risks. Once these risks are formalised on balance sheets, the market will be forced to respond.
  2. Why will repricing be sudden (a ‘Minsky moment’)? The trigger is psychology, not physics: the market responds not to gradual climate change, but to a sudden shift in risk perception. The catalyst could be the withdrawal of major insurers from a region, a series of devastating disasters, a downgrade of a country’s credit rating or a political decision. The result is a collapse in the prices of ‘toxic’ assets (real estate in risk zones, shares in vulnerable companies and businesses in high-risk regions), which will lose liquidity and access to insurance and credit.
  3. Repricing will be two-sided.

    Negative repricing (loss of value): will affect assets whose profitability depends on a stable climate and geographical location — real estate in flood and wildfire zones, agriculture in drought-prone regions and outdated infrastructure — as well as sectors linked to the main sources of GHG emissions (fossil fuels and agriculture)

    Positive repricing (increase in value): capital will seek ‘climate havens’. Assets that provide resilience will appreciate: providers of adaptation solutions (clean energy, energy-efficient materials and water technologies), companies with climate-resilient business models and real estate in safe regions.

Investor takeaway

The question is not whether repricing will happen, but when it will happen and which side your capital will be on. Ignoring this risk means betting that the ‘bubble’ will not burst. A viable strategy is to invest in assets that will benefit from this repricing. At the same time, the foundation of every strategy should be mitigating impacts worldwide (reducing emissions) and adapting to them.

07.2 Real estate

Real estate: repricing in real time

From sharp declines in house prices to insurance problems, climate change is already affecting real estate markets worldwide. Climate-related risks became ‘a deciding factor in home-buying decisions’ for more than 80% of prospective buyers on Zillow [Zillow, 2024]. Tellingly, 14 months later Zillow hid the feature from its website following complaints from estate agents and homeowners that it was hurting sales.

  • Increased flood risk can create tipping points at which house prices collapse suddenly [EEA, EUCRA 2024 / Van Ginkel et al., 2022].
  • Spain: each additional day above 35 °C reduces the sale price by €1.40 per m² and monthly rent by €0.0059 within the same province. With around 700,000 transactions in 2024, this equates to ~€117.6 million in annual losses on property sales. Yet in Spain’s cooler regions, higher temperatures actually increased prices (+€2.80/m²) — a climate-driven redistribution of value [Euronews, 2025].
  • England: each degree of warming allows the atmosphere to hold approximately 7% more water vapour, increasing the likelihood of intense rainfall. Some 6.3 million homes are already in areas at risk of flooding from rivers, the sea or surface water. Uncertainty ‘ripples’ through the market: two similar homes a few blocks apart attract different levels of interest simply because one is in a risk zone [Euronews, 2025].
  • United States: by 2055, 84% of areas may face declining property values due to climate risks, with an aggregate loss of $1.47 trillion in asset value. California was the first state to require sellers of homes built before 2010 to disclose a property’s wildfire risk. In Florida, 36% of respondents have moved or are considering moving because of the threat of hurricanes, floods and extreme heat [FSF, Property Prices in Peril, 2025; Euronews, 2025].
Investor takeaway

In regions where climate risks are already materialising or are projected to do so in the future, real estate risks losing its status as a safe-haven asset.

07.3 Mispricing the largest asset class

Failure to price climate risks correctly

The models the market relies on systematically understate climate risk, so key assets may be mispriced:

Investor takeaway

Risks are underestimated at every level. Assets may be repriced if they are valued without accounting for actual cascading damage: European investors are exposed not only to drought in Spain, but also to flooding in Thailand (through supply chains) or a hurricane in Florida (through catastrophe bonds). The system appears to be permeated by cascading risks, many of which remain difficult to measure.

07.4 Modelling BISThe bank for the world's central banks · ‘Climate Minsky Moment’

Repricing ‘dirty’ assets during a rapid energy transition

The mechanism of a ‘Climate Minsky Moment’: an abrupt tightening of climate policy (for example, a high carbon tax) devalues assets in ‘dirty’ sectors (such as fossil fuel extraction, conventional energy and heavy industry); banks that hold these assets or have lent against them suffer a decline in capital, triggering panic and fire sales and potentially leading to a deep crisis.

However, BISThe bank for the world's central banks states: ‘our results firmly reject the idea that financial stability considerations provide a valid reason to delay the transition to net zero’. Delaying is more dangerous — it only increases the scale of the future shock.

Annual probability of a systemic financial crisis (model by BISThe bank for the world's central banks)

[BIS, Charts 1–2, pp. 21–22]

Now · ‘slow’ policy~2.2%baseline under the current pathway
Short term · abrupt transition~2.7%under a sudden shift to ambitious policy (Paris targets), risk rises by nearly 25%
Long term · after the transition~1.4%an economy with a high carbon tax requires less capital; its financial sector is smaller, less leveraged and more resilient
Investor takeaway
  1. Analysts corroborate the repricing thesis. The risk of a sudden collapse in the prices of ‘dirty’ assets is not merely a theoretical assumption, but a scenario — the Climate Minsky Moment — modelled in detail in macroeconomic research by analysts at BISThe bank for the world's central banks.
  2. The risk comes from policy, not only from climate change. The threat to a portfolio may materialise not through physical damage from a hurricane, but through the abrupt, unexpected imposition of stringent taxes or quotas (transition risk).
  3. Delaying decarbonisation only magnifies the shock. The study’s own authors reject the ‘let’s wait’ argument: delay does not protect the economy, but instead necessitates more disruptive measures in the future, multiplying the likelihood of financial collapse. Proactive portfolio management can reduce these risks.
Investor takeaway

When the world’s largest and most conservative investors — central banks — begin systematically selling some assets and buying others, this can create a powerful long-term trend. Failing to account for climate risks puts a portfolio at odds with central-bank strategies: their actions to ‘green’ reserves may exert systemic pressure on the market, potentially raising the value of ‘green’ assets and reducing the appeal of ‘dirty’ ones.

Part 8

Audit and Repricing

Rating agencies and auditors: how climate considerations are being incorporated into credit analysis and mandatory financial reporting.

Part 8 · 2 themes

08.1 Rating agencies

Rating agencies: climate risk and creditworthiness analysis


Understanding of climate risks is only beginning to take shape

Major agencies are building a methodological framework and beginning to apply it, but label their analyses as ‘research’ because of the high degree of uncertainty. New scenario-analysis methods are needed, as this approach ‘can provide insight into possible outcomes and identify potential vulnerabilities’ [S&P Global, 2025S&P Global — Credit FAQ: How the Global Climate Policy Pendulum Could Affect Our Ratings (2025)“provide insight on possible outcomes … highlight potential vulnerabilities”]; ‘the current model does not capture the full scope of future threats’ [Fitch, SCVS, 2025Fitch — Sovereign Climate Vulnerability Signals / SCVS (2025)“SRM will not necessarily fully capture climate risks … full impact ... has not yet materialised”].

Fitch has published a ‘discussion paper’ — a roadmap for assessing the impact of physical climate risks on sovereign ratings — sending the market a clear signal that it is developing a tool that will systematically identify vulnerable countries [Fitch, SCVS, 2025]Fitch — Sovereign Climate Vulnerability Signals / SCVS (2025)“use Climate.VS as a screening tool … does not necessarily mean it will result in a downgrade”. The market will be forced to reprice when agencies begin systematic downgrades — for example, when a series of major disasters makes physical risks obvious and undeniable. We are on the threshold of that moment.

Investor takeaway

Leading rating agencies publicly state that new methodologies are needed because their current models cannot fully assess future climate risks. This signals that some risks are not yet fully reflected in current credit ratings or asset prices.

08.2 Auditors and new standards

Auditors and new standards: PRA, IFRS S1/S2 and the ‘sixth C’

The market will reprice companies based not only on profitability, but also on the quality of their climate reporting and the resilience of their business models.


New rules: IFRS S1/S2 — a generational shift in reporting

Regulators are beginning to require companies to assess and disclose both how they affect the climate and how climate risks affect them; the process is phased and will expand [Moody's, 2025Moody's — Climate Pathways (2025)“regulatory bodies globally are broadening climate disclosure requirements … company’s impact on climate change and climate change’s impact on the company”; Deloitte, 2024Deloitte — Sustainability and Climate Risk Assessment (2024)“regulatory disclosure requirements such as those from the TCFD, ISSB, and CSRD”]. Investors increasingly expect climate risks to be accounted for in financial statements, challenging the widespread assumption that climate change has no material, quantifiable impact on the valuation of assets and liabilities [KPMG, 2025]KPMG — On the 2025 audit committee agenda (2025)“Regulators, investors … increasingly expecting companies to consider climate risks when preparing their financial statements”.

‘The introduction of the new IFRS S1 (sustainability-related disclosures) and S2 (focused exclusively on climate-related disclosures) standards is being described as a generational shift in financial reporting’ — a fundamental change that is already under way [EY, 2025EY — Good Group: Illustrative climate-related disclosures (2025)“referred to as a generational change in financial reporting … IFRS S1 … IFRS S2”]. Audit committees must assess how climate risks (physical and transition) affect the value of assets and liabilities; climate-related and conventional reporting data must be aligned [KPMG, 2025KPMG — On the 2025 audit committee agenda (2025)“Regulators, investors and other bodies are increasingly expecting companies to consider climate risks when preparing their financial statements”; PwC, 2024PwC — The impact of climate change on financial statements (2024)“assessed the impact of climate change on measurement of assets and liabilities”“significant judgements and estimates ... climate-related risk”; EY, 2025EY — Applying IFRS: Accounting considerations for climate-related matters (2025)“measurement and disclosure of climate-related matters”“climate risk ... may impact a number of areas of accounting”“fair value measurements ... consider the relevant climate-related risk factors”].

The standards are rapidly becoming mandatory: 30 jurisdictions are already adopting ISSB S1/S2; together they account for almost 57% of global GDP. Companies will have to disclose Scope 1, 2 and 3 emissions; non-compliance means fines and a higher cost of capital [BIS, Climate-aware investing, 2025].

Reference: Scope 1, 2 and 3 emissions and implementation timelines by jurisdiction What are Scope 1/2/3, and when does mandatory reporting take effect in the United States, the European Union, the United Kingdom, California, Singapore and Switzerland? Expand
  • Scope 1 (direct): emissions produced by the company itself — from its factories or vehicles.
  • Scope 2 (energy-related): emissions generated at the power plants from which the company obtains electricity or heat.
  • Scope 3 (indirect): all other emissions associated with the company’s activities but occurring beyond its direct control: emissions from suppliers and the logistics chain, from the use of its products, and from companies in which it invests or to which it lends.

Indicative timelines for mandatory climate reporting:

  • United States (SEC): from 2026 — the largest public companies (reporting for 2025; implementation has been suspended, in line with Trump’s policies).
  • California (SB 253 and SB 261): from 2026 — all large companies (public and private, reporting for 2025).
  • European Union (CSRD/ESRS): from 2025 — large companies that previously filed non-financial reports (reporting for 2024); from 2026 — other large companies.
  • United Kingdom (TCFD-aligned): from 2022 — the largest public companies and financial institutions; from 2023–2024 — large public and private companies, including those listed on AIM.
  • Singapore (SGX / ISSB-aligned): from 2026 — all listed companies (reporting for 2025).
  • Switzerland (TCFD-aligned): from 2025 — large public companies and financial institutions (reporting for 2024).

08.3 Repricing through compliance

Repricing will be formalised

The entire system of International Financial Reporting Standards (IFRS), reinforced by the IFRS Foundation’s S1 and S2 requirements, now aims to compel companies to quantify climate risks and reflect them on their balance sheets through specific accounting procedures (impairment, remeasurement of liabilities and credit-loss provisions). Regulators, banks, auditors and asset managers will require, scrutinise and challenge climate-related estimates and assumptions — these risks can no longer be ignored on balance sheets.

Likely consequences:

  • Repricing through write-downs (impairment): write-downs directly reduce the carrying value of assets and companies’ capital.
  • Higher cost of capital: due to higher climate risks or energy-transition risks.
  • Reduced earnings: direct physical damage, rising insurance costs, supply-chain disruptions, declining labour productivity and carbon taxes.
  • Higher operating and capital expenditure: the need to invest in adaptation, relocation or the energy transition.

When companies, under pressure from auditors and regulators, begin to acknowledge that their factories, infrastructure and other assets are worth less because of climate risks (or accelerate climate change through their emissions), this could materially affect their capital and share prices. By contrast, companies that demonstrate low vulnerability to climate and energy-transition risks, as well as the least negative impact on the climate, may rise in value. Companies that cannot provide reliable, audited data at all are also likely to be penalised by the market. The market has not yet repriced these risks because most companies have not reflected them in their financial statements; new disclosure rules and audit requirements may trigger this repricing in the coming years.


The market as a risk amplifier

Investors’ expectations regarding climate scenarios affect the cost of capital and companies’ investment decisions [EUCRA, 2024European Environment Agency — European Climate Risk Assessment (2024), ch. 17“Investors' expectations on the realisation of climate scenarios affect the cost of capital and thus firms' investment decisions…”Website]. If climate risks have gone undisclosed for a long time, the first comprehensive disclosure or a major disaster could trigger sharp asset repricing. In such a situation, urgent sell-offs (fire sales) are particularly damaging to investor returns [EUCRA, 2024European Environment Agency — European Climate Risk Assessment (2024), ch. 17“Fire sales can be particularly harmful to investors' returns…”Website], while financial links among banks, funds and insurance companies (cross-shareholdings, loans and deposits) increase the risk of a chain reaction (contagion) [European Commission, 2024European Commission (2024)Investment funds and insurers are closely linked to the banking sector through cross-shareholdings, loans, common exposures and deposits.]. A similar mechanism underpinned the 2008 crisis.

Investor takeaway

There is a narrowing window before risks are reflected in credit spreads and market prices: a viable strategy is to exit assets destined to become ‘toxic’ early and move into those that will benefit from repricing.

Part 9

Regions and risks

Two divides — latitudinal and wealth-based · regional matrix · the case of Cyprus

Part 9 · 2 themes

09.1 Introduction · geography of risk

Two divides: latitudinal and wealth-based

Climate risks and impacts are distributed extremely unevenly around the world, and each region requires its own detailed analysis. The broad pattern comes down to two divides.

  1. The latitudinal divide. The south suffers primarily from heat and drought, while the north faces extreme rainfall and flooding. The difference is apparent even within a single country or bloc — the US, Europe or Ukraine: economic losses and physical risks in southern and northern areas may differ severalfold.
  2. The wealth-based divide. Poor countries and regions are the most vulnerable: they lack the resources for recovery, adaptation and the energy transition. Southern countries, where it is already hot, reach levels of heat that are unacceptable for human life and economic activity sooner.

At the same time, regions are linked by a shared atmospheric system: for example, the disruption of the stratospheric polar vortex over the Arctic intensified extreme rainfall in southern China [Arctic stratospheric polar vortex collapse amplified South China extreme rainfall, 2025]. There are no completely isolated, ‘safe’ countries — climate change affects every country to some extent.

№1The US — the world's highest absolute economic losses from weather events[Bloomberg, The Climate Economy Outlook, 2025]
x2Europe's climate is changing at about 2× the global average rate[EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)]

09.1 Introduction · geography of risk

Europe: shifting economic activity and the ‘Two Europes’

Europe is unprepared for rapidly accelerating climate risks, several of which have already reached critical levels. Policy action is lagging far behind the pace at which the threats are growing [EEA, EUCRA, 2024].

The greatest economic damage comes not from one-off disasters but from persistent, chronic impacts of climate change: recurring heatwaves, lost working hours and rising energy costs for cooling buildings and critical infrastructure such as data centres [JRC]. For example, in 2022 the temperature in the UK exceeded 40°C for the first time on record: railway tracks buckled and runways melted [JRC PESETA V, 2025JRC — Regional economic climate risks in Europe (2025)], because much of Europe's infrastructure was designed for the former climate, and every climate record subjects it to stresses it was not built to withstand.

A climate-driven shift in economic activity is under way: tourism is moving north, while agriculture in the south, on which the rest of Europe partly depends, faces an existential threat. This is creating both clear losers and potential, less obvious winners.

Climate change amplifies economic inequality. The greatest damage will fall on already more vulnerable coastal, Mediterranean and Eastern European regions [JRC]. Poorer regions with ageing populations and a dependence on ‘dirty’ industries may face a ‘perfect storm’ in which physical shocks trigger severe social and economic crises, increasing credit and sovereign risks.

  1. Potential ‘Winners’ — resilient, developed regions (southern Germany, Scandinavia and Austria). They attract investment and skilled professionals for the ‘green transition’; their economies are sufficiently diversified to withstand a shock, and their financial capacity allows them to invest in adaptation. They could become ‘climate havens’ if they invest in adaptation and the energy transition.
  2. Potential ‘Losers’ — vulnerable, lagging regions: Southern Europe (water stress) and Eastern Europe (‘carbon traps’, public-health problems). A double burden: the highest costs of moving away from fossil fuels and the most severe physical impacts. The key risk is a vicious circle: these regions need enormous investment for the transition and adaptation, but rising climate and social risks make them less attractive to capital.
Investor takeaway

A strategy of investing in ‘Europe’ as a single asset no longer works. The climate transition requires a fundamental repricing of regional risks.

Adaptation policy is becoming a prerequisite for the financial stability of vulnerable regions; those that fail to adapt will face a risk of financial destabilisation [JRC, PESETA V, 2025].

Regional matrix

Regional matrix: threats · current situation · scenarios
RegionKey threatsAlready happening +1.5°Outlook +2° / +3°Financial implications
US Droughts and wildfires, hurricanes, severe convective storms (tornadoes, hail) The world's highest absolute losses; droughts, fires, hurricanes and floods remain among the main channels of damage [Bloomberg, 2025] By mid-century: PIK estimates a median income decline of about −8% for North America; NBER estimates the peak regional effect of a global temperature shock at close to −10% for North America and Europe [NBER, 2026NBER (revised) — The Macroeconomic Impact of Climate Change: Global vs. Local Temperature (2026)“The peak effect in North America and in Europe is near −10%, albeit not very precisely estimated.”; PIK revised version, 2025PIK — The economic commitment of climate change, revised (2025)“permanent income reduction for the majority of regions, including North America and Europe (with median income reductions of approximately 8 and 7% respectively)”] ‘Uninsurable zones’ are already a reality (California, Florida); migration and development continue into high-risk areas
Mid-latitudes of the Northern Hemisphere Concurrent heatwaves, compound heat and drought, synchronous agricultural shocks Over the 1979–2019 period, the frequency of concurrent heatwaves increased by a factor of 6, their average spatial extent by 46% and their maximum intensity by 17% [FAO & WMO, 2026] Compound ‘extreme heat + drought’ events have already become more severe; by 2081–2100, their frequency across most land areas may increase by 200–300% relative to 1986–2005 [FAO & WMO, 2026] Diversifying supplies ‘by region’ loses some of its protective value if several breadbaskets are hit simultaneously
Southern Europe Heat, droughts, water scarcity, fires The impact of heatwaves on GDP reaches −1.1–1.4 percentage points [Allianz, 2025Allianz — Heatwaves: Economic ImplicationsWebsite]; about 30% of Southern Europe's population lives in regions already facing chronic water scarcity; in summer, this share rises to about 70% [EEAEEA — Use of freshwater resources in EuropeWebsite] At +2 °C: river flow on low-flow days −40% (southern Spain, Portugal, Greece and France) [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)PDF · Chapter 5, p. 129]; at +3 °C the risk to people and the economy becomes ‘catastrophic’ [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)]; heat that occurs ‘once every 50 years’ — almost every year in Spain and parts of Portugal [JRC PESETA IV, 2020JRC PESETA IV — Heat and cold extremes (2020)“In a 3°C warmer climate compared to pre-industrial times, a current 50-year heatwave may occur almost every year in Spain and parts of Portugal, every 3 years in most other southern European areas and at least every 5 years in other regions of Europe.”“At 2°C, this further grows to 172 million/year.”PDF · p. 3] Agriculture and tourism — pillars of the economy — depend directly on water; risk of ‘hard limits to adaptation’
Central and Western Europe River flooding (50% of all weather-related losses [Swiss Re, 2024]), heat, low river levels, megadroughts 2021 floods (Germany/Belgium): €44 billion; Rhine, 2018: 132 days of shipping disruption, −0.4% of German GDP [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024); JRC Atlas] Water scarcity is spreading to the EU's industrial core; coastal flooding at +3 °C — more than €1 trillion a year [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)] Ageing infrastructure designed for the former climate; logistics depend on rivers (Rhine, Danube)
Northern Europe Droughts (a new phenomenon), floods, storms 2018: Scandinavian hydropower below normal, water shortages even in Finland and Sweden [EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)]; Scotland-2025: reservoir levels 40% below normal; UK-2022: 40 °C for the first time Summer rainfall in England: −15% by the 2050s, −22% by the 2080s [Open University → EEA, EUCRA, 2024EEA — European Climate Risk Assessment, EUCRA (2024)] The ‘illusion of a safe North’ has been dispelled: infrastructure was not designed for drought, and damage in ‘unexpected’ places is disproportionately high
Eastern Europe Floods, heat, ‘carbon traps’, air pollution Romania, Latvia and Bulgaria are among the 5 EU countries with the highest average annual flood losses; damage from major events reaches 7–17% of GDP [World Bank, 2021World Bank — Economics for Disaster Prevention and Preparedness in EuropeWebsite] Rising credit and sovereign risks due to the combination of physical shocks and transition costs [JRC]
Emerging economies Heat, droughts, floods, cyclones Insurance gap: 94% of losses in China, 93% in India and 83% in South Africa are uninsured [Allianz, 2025]; India: 82% of newly irrigated land is in water-scarce areas [Nature Water, 2024] Regional sequences of extreme events: losses of up to 12.5% of GDP (Africa) [NGFS, 2025]; by 2050, droughts may affect more than three-quarters of the world's population [UNDRR, 2025] Almost all losses are borne by public budgets and households; access to capital for adaptation is limited

Regional case study

The case of Cyprus


09.2.1 Case study: Cyprus

Note: There are still no comprehensive models capable of accounting for all cross-system and cascading effects (spillover effects). The reality may therefore be more severe: climate processes may unfold faster, reach higher levels of intensity and be accompanied by phenomena not previously accounted for.


Epicentre of warming

The Mediterranean region, like Europe as a whole, is warming at 2× the global average rate [Cyprus NASCyprus National Adaptation Strategy“EMME is warming nearly twice as fast as the global average especially during summer, while alterations in the hydrological cycle, primarily through reduced precipitation, have become increasingly evident.”PDF · p. 26]. Major climate risks, including wildfires, floods, water scarcity and coastal erosion, are already damaging Cyprus's biodiversity, agriculture, aquaculture and fisheries, underscoring the urgent need for stronger prevention measures [European CommissionEuropean Commission — Country Report: Cyprus“Significant climate risks (e.g. wildfires, floods, water scarcity and coastal erosion) are harming Cyprus’s biodiversity, agriculture, aquaculture and fisheries sector, thus underscoring the urgent need for improved prevention.”Website].

Already happening

Hot days (>35 °C) x2 Twofold increase: the average annual number of days above 35 °C rose from 9.4 (1950–1979) to 19.3 (2015–2024). The record was set in 2024, with 33 hot days (ERA5 area-wide average; values for individual locations may be higher) [World BankWorld Bank Climate Change Knowledge PortalERA5 Historical Data: Observed Timeseries of Annual Number of Hot Days (T-max > 35°C) in Cyprus (1950-2024).Website].
Extreme heat (>40 °C) x3,9 Increase by almost a factor of 4: the average number of extremely hot days rose from 0.11 (1950–1979) to 0.43 per year (2015–2024) (ERA5 area-wide average; values for individual locations may be higher) [World BankWorld Bank Climate Change Knowledge PortalERA5 Historical Data: Observed Timeseries of Annual Number of Hot Days (T-max > 40°C) in Cyprus (1950-2024).Website].
Mediterranean Sea +1,4°C Warming waters: Marine heatwaves have shifted from episodic to annual and have been classified as at least ‘strong’ for 3 consecutive years (2023–2025). This poses a risk to marine ecosystems and tourism [ESOTC, 2025Copernicus ESOTC 2025“Sea surface temperature — Increase since the 1980s: Global (60ºS–60ºN) +0.6ºC; WMO RA VI (Europe) +1.1ºC; Mediterranean Sea +1.4ºC.”PDF · p. 11].

Increase in tropical nights (Tmin > 20°C)

Night-time heat hinders physical recovery, increasing health risks for residents and tourists.

Uneven regional warming

Rising temperatures have affected the island unevenly. In Nicosia (centre), Larnaca (south) and Polis Chrysochous (north), a sharp increase in the number of hot days (>35 °C) has been recorded relative to the 1986–2005 baseline. In mountainous Agros the increase is also significant, though less pronounced. By contrast, in Paphos (west) and mountainous Prodromos only a slight increase has been recorded.


Wildfires

Cyprus faces a significant and steadily rising wildfire risk. The island has the highest level of fire danger among all Mediterranean islands and ranks second in Europe for burnt area as a share of its territory. The probability of weather conditions that could cause fires threatening life and property is estimated at more than 50% in any given year [World Bank, 2024World Bank Group: Country Climate and Development Report for Cyprus (2024)“Cyprus faces a significant and increasing risk of wildfires... Cyprus faces the highest wildfire danger among Mediterranean islands and ranks second in Europe for burned area per land mass... The likelihood of weather conditions leading to wildfires that can cause loss of life and property is estimated to be greater than 50 percent in any given year.”Link].

Climate change has already made extreme fire weather conditions (FWI) in Cyprus 10× as likely [State of Wildfires 2024-25State of Wildfires 2024-25“FWI values recorded in Türkiye, Cyprus and Greece were 10 times more likely due to climate change. The FWI values recorded in Spain and Portugal were 40 times more likely...”PDF · p. 41].

In 2025, Cyprus experienced the worst fire season in its history. It was marked by extreme conditions, including a severe heatwave and dry weather. As a result, an area almost the size of Nicosia [2026 Country Report2026 Country Report - Cyprus“The 2025 wildfire season in Cyprus was marked by extreme conditions (including a severe heatwave and dry weather) that resulted in the worst wildfire in Cyprus’s history, burning an area almost as large as Nicosia.”PDF · 2026]was burnt. Around 900 private propertieswere destroyed, and total direct damage is estimated at €252.68 million [European CommissionEuropean Commission — Mobilisation of the European Union Solidarity Fund, COM(2026) 1002 final“The Cypriot authorities estimate the total direct damage caused by the disaster at EUR 253.69 million. The Commission accepted EUR 252.68 million as plausible total direct damage.”“Several schools and health establishments had to reduce their services and close to 900 private properties were destroyed.”PDF · 18 May 2026].

The events of 2025 continue a trend of escalating risk:


Freshwater crisis

Cyprus already faces acute, chronic water scarcity, and its water exploitation index is the highest in the EU [Country ReportEuropean Commission — Country Report: Cyprus“Cyprus faces severe, chronic water scarcity and its water exploitation index indicates the highest pressure in the EU as a whole.”PDF]. Meanwhile, droughts and water scarcity will only worsen, placing extreme pressure on the population and infrastructure [EPRS, 2025European Parliamentary Research Service (Feb 2025)“Water scarcity and drought in particular are expected to worsen, putting further pressure on human life and ecosystems... lack of sustainable water management to build resilient agriculture is of particular concern.”PDF · pp. 2, 4]. The rapid physical depletion of natural water resources is therefore a key risk.

In 2026, reservoir levels reached their lowest point in the 125-year observational record even before the tourist season began [Copernicus, 2026EU Space: Copernicus Image of the Day“Severe drought in Cyprus, February 2026”Website]. The authorities urged the public to cut water consumption by 10%, while the 2026 allocation of water for agricultural irrigation was reduced by one-third [Euronews, 2026Euronews“Cyprus water emergency: citizens urged to reduce water use as dams reach record low” (Jan 2026).Website].

Near-total dependence on desalination:

The country has shifted almost entirely to desalination: around 80% of all drinking water on the island — up to 245 thousand cubic metres per day — is supplied by energy-intensive desalination plants [WDD CyprusWater Development Department (Ministry of Agriculture, Cyprus)Official data: Permanent and mobile desalination plants now cover approx. 80% of the island's drinking water needs.]. Desalination is critically dependent on electricity, creating a potential cascading risk.

01 · The cost of desalination Dependence on the power grid Desalination reduces dependence on reservoirs but makes the water supply dependent on a stable electricity supply. In hot weather, when demand peaks and reserve capacity is limited, this creates a cascading risk: a power failure can quickly become a water-supply failure. [Xevgenos et al., 2021Desalination and Water Treatment — Cyprus as a case study“In 2018, 69.6 million m³ of desalinated water were produced in Cyprus requiring the consumption of around 240.9 GWh of electrical energy...”DOI: 10.5004/dwt.2021.26916].
02 · The cost of desalination Hypersaline brine discharge After desalination, hypersaline brine — water with twice the salt concentration — is discharged back into the sea. In 2018, 69.6 million m³ of desalinated water generated 103 million m³ of brine. Hypersaline brine is a serious problem because it degrades marine ecosystems and creates dead zones in the sea. This is a direct environmental and economic risk to coastal tourism, fisheries and biodiversity. [CORDISCORDIS — Striving for more environmentally friendly drinking water on Cyprus“We found negative effects on Posidonia oceanica seagrass meadows within around 150 metres from the discharge point.”].
03 · The cost of desalination Impact on property development Because desalination costs are rising, the government explicitly states that water-intensive development, including resorts and golf courses, must be restricted by law. The National Adaptation Plan openly acknowledges that investor lobby groups are the main obstacle to this ban [Cyprus Action PlanNational Climate Change Adaptation Action Plan 2025–2050PDF].

Energy

Critical vulnerability Single
point
of failure
electricity underpins the island's water, cooling and operations
Core risk logic

Electricity is not a sector; it is the backbone of Cyprus: building cooling, water supply, desalination, pumps, hospitals, communications, hotels and trade all depend on it. A climate shock to the energy system therefore quickly becomes a shock to several sectors at once [EEAEuropean Environment Agency — Climate risks in energy systems“A stable and affordable energy supply is central for a modern society — Risks to energy supply can cascade to all societal sectors and activities, threatening security, economic well-being, and human health.”PDF · 2024].

Vulnerability profile Cyprus's energy system is simultaneously isolated, import-dependent, poorly diversified and vulnerable to climate risks
0 external grid reserves

Cyprus remains the only EU member state isolated from the internal energy market. At times of peak demand or a capacity shortfall, it cannot import electricity from a neighbouring grid.

87,7% energy import dependence

The country's entire energy base depends on imported fuel. A price or logistics shock affecting oil can spread across the entire energy-dependent system. Cyprus is one of the EU member states most dependent on oil

868 MWVasilikos
49%of capacity

All three plants account for 83% of installed capacity. This leaves the system poorly diversified.

Climate mechanism Heat compounds three risks: demand, reserve capacity and generation

This is dangerous for an isolated grid: when the island needs maximum capacity, the system's reserve capacity may disappear.

Trigger Heat more hot days, hot nights and heatwaves
Demand spikes ↑ Heat often causes a sharp increase in grid load

During the 2025 heatwave, electricity demand in Europe jumped by as much as 14%, exceeded normal peaks and became one of the factors behind outages in Italy [WRIWorld Resources Institute — Europe’s Soaring Heat and the Air Conditioning Dilemma“During the June and July 2025 heat wave... electricity demand in some parts of Europe spiked by as much as 14%, peaking above typical winter levels and contributing to outages in countries like Italy.”Website · 2025].

Cascading effect A grid failure spreads to water, cooling and the economy

The problem extends beyond electricity: the very systems needed during heat and drought are put at risk.

03 · Economy Hotels, trade, communications

Power-supply risk spills into other sectors: such failures threaten safety, economic well-being and health [EEAEuropean Environment Agency — Climate risks in energy systems“Risks to energy supply can cascade to all societal sectors and activities, threatening security, economic well-being, and human health.”PDF · 2024].

Investor takeaway The danger lies not only in individual risks but also in their combination and potential cascading impacts

Water and energy systems depend on climatic conditions and have virtually no spare capacity. An energy failure in Cyprus could therefore become a water, sanitation, tourism and operational failure all at once.

Future

Climate

Cyprus will face significant temperature increases and declining precipitation in both the near and distant future. [Cyprus NASCyprus National Adaptation Strategy“Cyprus is projected to experience significant increases in temperature and decreases in precipitation in both the near (2041-2060) and distant (2081-2100) future.”PDF · p. 26]


Timing: mid-century under older projections; according to new data, the risk could materialise in just 10–12 years:

Optimistic scenario (RCP4.5, +1.6 °C).

Pessimistic scenario (RCP8.5, +2.1 °C)


Timing: end of the century under older projections; according to new data, the risk could materialise in just 25–35 years:

Optimistic scenario (RCP4.5, +2.1 °C).

Pessimistic scenario (RCP8.5, +4.1 °C)


Food

Cyprus has no strong domestic food buffer: agriculture is already constrained by water scarcity and heat, while food imports depend on external suppliers, including Greece and Italy [2026 Country ReportEuropean Commission — 2026 Country Report: Cyprus“The agricultural sector is challenged by water scarcity and heat stress, which are impacting crop yields and food security.”PDF · p. 81; WITSWorld Bank WITS — Cyprus Food Products Imports by country, 2023“In 2023, the top partner countries from which Cyprus Imports Food Products include Greece, Italy, Germany, United Kingdom and Argentina.”Website · 2023].

Local harvest Crop yields are already under pressure: water scarcity and heat stress are harming agriculture, crop yields and food security [2026 Country ReportEuropean Commission — 2026 Country Report: Cyprus“The agricultural sector is challenged by water scarcity and heat stress, which are impacting crop yields and food security.”PDF · p. 81]
Desertification 91% Almost the entire territory is vulnerable: 91% of Cyprus lies in critical or sensitive zones vulnerable to climate change and desertification [Audit OfficeAudit Office of the Republic of Cyprus — Water resources and climate change“Increase in the frequency and intensity of droughts. 91% of Cyprus is characterized as critical or sensitive to climate changes.”PDF · p. 4]

Imports do not eliminate the risk: Cyprus's key food suppliers include Greece and Italy, which are in the same climate-vulnerable Mediterranean region [WITSWorld Bank WITS — Cyprus Food Products Imports by country, 2023“In 2023, the top partner countries from which Cyprus Imports Food Products include Greece, Italy, Germany, United Kingdom and Argentina.”Website · 2023; JRCJoint Research Centre — Climate impacts on the Water-Energy-Food-Ecosystem nexus in Europe“The Mediterranean region faces significant challenges in meeting irrigation demands in current climate (1981-2010), leading to increasing water scarcity and stress.”PDF · 2026]. Climate change is expected to reduce crop yields in other regions as well; there is also a risk of global food shocks. (See the Food chapter).

Local production losses are substantial: Cyprus is among the EU areas experiencing the largest relative declines in wheat yields due to drought, alongside Spain, Romania and southern Italy. Heat and water scarcity are already reducing crop yields, raising costs and threatening food security [European Commission, 2026Cyprus 2026 Country Report (SWD(2026) 213)“Heat and water stress are already reducing yields, increasing costs, and threatening food security...”PDF] [EEA, 2025Europe’s environment and climate: state and outlook 2025“Significant reductions in yields of wheat due to droughts are projected at 2°C of warming, with the highest reductions in percentage terms expected in Spain, Romania, southern Italy and Cyprus.”PDF · p. 37].

This double physical shortage — locally and among suppliers — could therefore translate into significant inflation. As a result, Cyprus is expected to see one of the EU's largest increases in household food expenditure, and — alongside Greece — the largest increase in healthcare expenditure due to climate change [EPRS, 2025European Parliamentary Research Service (Feb 2025)“A study on the cost of climate change... estimates that the highest increase in climate-induced health expenditure is expected to occur in Cyprus, as well as in Greece. Cyprus is also among the countries with the highest increase expected in household food expenditure.”PDF · p. 6].


Sea-level rise and tourism

Tourism is a vital pillar of Cyprus's economy: around 20% of GDP is linked to the sector directly or indirectly [Trade.govU.S. International Trade Administration“Travel and tourism-related activities generate approximately 20 percent of ROC GDP” (2026).Website]. Yet the sector depends critically on coastal ecosystems, which are now degrading rapidly. More than 90% of tourists choose coastal towns, while pronounced seasonal peaks significantly intensify water stress and overload infrastructure [2026 Country ReportEuropean Commission — 2026 Country Report: Cyprus“Coastal tourism is highly seasonal, leading to environmental degradation, water stress, and infrastructure overload during peak months...”PDF · p. 109].

In addition to extreme heat and freshwater scarcity, sea-level rise and the associated coastal erosion pose a physical threat to tourism in Cyprus. Coastal infrastructure in Cyprus is not yet subject to systematic climate assessment, even though sea-level rise is projected to cause annual losses of up to 0.4% of GDP by 2050; timely adaptation could reduce these losses by 90% [EEAEuropean Environment Agency“The rising sea levels are projected to cause annual economic losses of up to 0.4% of gross domestic product by 2050. Strategic adaptation measures... could reduce these losses by up to 90%.”Website].

Underlying vulnerability 91% of beaches are already critically narrow — less than 50 m wide, with 42% narrower than 20 m. They have virtually no room to retreat inland. [Monioudi et al., 2023Monioudi et al. (2023)“...almost 42% recorded maximum 'dry' beach widths (BMWs) of less than 20 m and 91% of less than 50 m...”PDF · p. 6]
Storm inundation (by 2050) 54% of beaches will, during storms under the RCP8.5 scenario, be completely covered by water, with inundation extending beyond their present width. By 2100, this share will reach 72%. [Monioudi et al., 2023Monioudi et al. (2023)“...whereas under RCP 8.5, more beaches (43, 49 and 54%, respectively) will retreat more than their current BMWs.”PDF · p. 10]
Irreversible loss (by 2100) 72% of beaches that are unprotected will be irreversibly eroded, permanently losing half their width because of the rise in baseline sea level under the RCP8.5 scenario. Under the moderate RCP4.5 scenario, this share will be 47%. [Monioudi et al., 2023Monioudi et al. (2023)“In 2100, about 47% and 72% ... of the 241 unprotected Cypriot beaches will be permanently eroded, due to mean sea level rise (SLR), to 50% of their present maximum width...”PDF · p. 1]

Economy


European Commission estimates: Cyprus ranks first in the EU for climate risk

Under the +2 °C scenario, Cyprus ranks first for economic damage among all 27 EU member states [JRC PESETA V, 2025JRC — Regional economic climate risks in Europe (2025)“A significant proportion of the population (more than 75%) in countries such as Greece, Cyprus, and Croatia are expected to suffer significant losses both of GDP and consumption.”“Countries are ordered by their average losses in the baseline.” (Figure 4, CY is far left)PDF · p. 13]. A report by the JRCEuropean Commission's Joint Research Centre divides the damage into two indicators: GDP decline (overall economic activity) and decline in consumption (a real fall in living standards and welfare, because unavoidable spending, such as repairing infrastructure after disasters, increases GDP but directly reduces household incomes). The charts show the following levels of risk to the population:

GDP decline at +2 °C>1%structural economic underperformance affecting almost 100% of the population
Decline in consumption at +2 °C2–5%lower real living standards affecting most of the population (~60%)
Decline in consumption at +2 °C5–12%the largest decline, affecting ~10% of the population

Model limitations:


Estimates by Cypriot research centres

Cumulative discounted losses to the island's economy by 2050, based on a scenario in which +2 °C is reached by 2050 (this threshold and the associated damage may arrive considerably earlier):

GDP damage at +2 °C€29 billionin cumulative losses to the island's economy, assuming warming by 2050. With large-scale investment in preventive adaptation — itself a cost — the damage could be limited to €4 billion [UCy, 2025Economics Research Centre of the University of Cyprus (UCy), Dec 2025“Cumulative discounted GDP losses under the Business-as-Usual (BAU) scenario are expected to be nearly €29 billion by 2050... However, with timely adaptation (SUS scenario), the losses can be limited to €4 billion by 2050.”]
Tourism damage at +2 °C€3.8 billionin cumulative losses to the flagship sector, assuming warming by 2050. With adaptation measures, the damage is limited to €500 million [UCy, 2025Economics Research Centre of the University of Cyprus (UCy), Dec 2025“The sectors hit hardest... Tourism: cumulative losses of €3.8 billion (BAU), reduced to €0.5bn (SUS) by 2050”]
Financial-sector damage at +2 °C€2.3 billionin cumulative losses to the financial-services sector, assuming warming by 2050. Agriculture will meanwhile lose €500 million [UCy, 2025Economics Research Centre of the University of Cyprus (UCy), Dec 2025“Financial services: €2.3 billion by 2050... Agriculture: €0.5 billion”]

Impact on the population: household spending on food, healthcare and electricity is projected to rise sharply. Cyprus is expected to become one of the EU countries where vulnerable groups are hit hardest [Cyprus Institute, 2025The Cyprus Institute — Policy Brief (2025)“Cyprus is expected to be one of the countries with the strongest negative impacts on vulnerable households due to climate change. Household expenditure on food, electricity and health services are projected to increase...”PDF · p. 8].


Physical risk

In addition to macroeconomic risks, investors face a direct physical threat to assets:

Investor takeaway

Cyprus's infrastructure is already operating at the limits of its heat and water resilience, while climate pressure will continue to grow. The current model of large-scale resort development is in direct physical and regulatory conflict with climate change.

The island should be stress-tested not simply as a ‘warm southern market’ but as an economy facing complex water, heat, wildfire and coastal risks. Assets tied to cheap water, the ‘sea–sun–beach’ model, wildfire-prone areas or low-lying coastlines should be priced to reflect substantial increases in the costs of adaptation, insurance and capital.


Adaptation: can the negative scenario be avoided?

Successfully withstanding climate shocks requires a large-scale transformation of infrastructure (for more detail, see the global ‘Adaptation’ section). In Cyprus, as in many other countries, this process is lagging far behind the pace of warming, partly because of insufficient funding and delays in policy implementation:

Investor takeaway

Cyprus is highly vulnerable to climate risks. Natural conditions will deteriorate, adaptation is not guaranteed, and the market repricing of climate risks (see ‘The Coming Repricing’) may occur well before the physical changes, as awareness grows of the level of the threats, the scale of future impacts and the cascading risks. From this perspective, Cyprus's outlook may prove uncertain. Either tourist flows, which account for 20% of GDP, or investment may stop growing or begin to decline, and asset values may be repriced.

Under such a scenario, buying property and even making medium-term investments may already be substantially riskier, particularly compared with some other regions to which capital may begin to flow as ‘climate havens’.

Part 10

Industries

Industry vulnerability matrix · supply chains (diversification is no safeguard) · beneficiary sectors.

Part 10 · 3 themes

10.1 Vulnerability matrix

Industry vulnerability matrix

Each industry requires a separate assessment that takes account of where it operates and of global interconnections, but economies rest on ecosystem services — food, water, energy and raw materials — as well as on regulatory frameworks. The climate crisis hits each of these foundations and then transmits the damage to the financial system through lower profits, damaged collateral, higher credit risk and insurance payouts [IFoA, 2024IFoA — Climate Scorpion (2024)“nature as an asset that provides ecosystem services to society, such as the provision of raw materials for our economy, the provision of food and regulating services like climate regulation.”“ecosystem services… provide the essentials that society requires in terms of food, water, a stable climate, and so on.”; IFoA, 2023IFoA — Biodiversity and Nature-related Risks for Actuaries (2023)“ecosystem services… underpin our economies, societies, health and food systems”“Provisioning services are goods obtained from ecosystems such as food, raw materials, freshwater, energy and medicines.”; Zeidy, 2023Zeidy — Climate Related Risks to the Financial Sector (2023)“climate change can damage physical collateral”“severe weather events… reduce corporate profitability and potentially increase credit risk to lenders”“Severe climate change will lead to increased insurance claims and liabilities.”].

Industry vulnerability: direct and financial risk
IndustryDirect vulnerabilityFinancial risk
AgricultureLower crop yields due to drought, heat and floods; dependence on water (70% of global water withdrawals)Inability to repay loans — a direct credit risk for banks with a large share of the agricultural sector in their portfolios
Fisheries and forestryDecline or loss of the production base; firesLoss of value in production assets and collateral
Real estatePhysical destruction of or damage to buildings due to fires, floods and hurricanes; land subsidenceDecline in the value of mortgage and commercial loan collateral — direct losses for banks
ConstructionMore stringent building requirements and standards; higher costs; fewer available sitesHigher costs as sales decline; pressure on margins
Transport and logisticsDestruction of ports, roads and airports; rivers drying up; disasters affecting transport routesSupply chain disruption across all industries; higher costs
Insurance and reinsuranceA sharp rise in the number and size of insurance payoutsInsurer bankruptcies — a systemic risk because banks are major creditors of insurers
Heavy industry and manufacturingProduction stoppages due to physical damage, logistics disruptions or power outages; high water intensity (steel, pulp and food processing)Lower profits; higher credit risk for banks
EnergyPower generation: extreme weather, overheating and water shortages for cooling thermal and nuclear power plants [IEAIEA — The world’s electricity systems must be ready to counter the growing climate threatWebsite]. Fossil fuels: transition risk and loss of value in oil, gas and coal assets [COMESACOMESA — Climate Change impact on the Financial SectorPDF].Asset write-downs on the balance sheets of banks and investment funds; greater risk of power-generation disruptions and higher infrastructure costs.
Tourism and recreationShifts in visitor flows; degradation of infrastructure and natural assets (beaches, reefs, forests and snow)Declining asset returns and falling values of resort property

Dual, cumulative risk

Decarbonisation is highly uneven: emissions from power generation (Power) are falling sharply and transport emissions are stabilising, while emissions from heavy industry (steel, cement and chemicals) and agriculture/land use continue to rise or remain high [Rhodium, Climate Outlook, 2025]. This creates a dual risk for industry and agriculture:

  1. Greatest transition risk: because these are the industries that are not decarbonising, they will become the main target of future climate regulation (carbon taxes and standards) — a direct threat to profitability.
  2. Greatest physical risk: it is the water-intensive industrial and agricultural sectors that suffer most from drought, water shortages and heat.

Unlike energy and transport, agriculture has no clear technological solutions: decarbonising it may be the hardest challenge. Companies in renewable energy and electric-vehicle manufacturing are ‘on the right side of history’; heavy industry and agriculture are the primary source of future risk. The financial sector is already quantifying this: ‘dry’ events (drought and heat) cause the greatest productivity losses and the largest increases in default probabilities in agriculture and capital-intensive industries, while the energy supply sector suffers considerably from both ‘dry’ and ‘wet’ events [NGFS, Short-Term Scenarios, 2025].

10.2 Beneficiaries

Likely beneficiaries: on the right side of repricing

The energy transition is the greatest opportunity for industrial growth since the Industrial Revolution [Boston Consulting Group, 2024]. It is a megatrend that will shape the economic landscape over the coming decades, whatever the short-term effects [S&P Global, 2025S&P Global — Credit FAQ: How the Global Climate Policy Pendulum Could Affect Our Ratings (2025)“climate transition is a megatrend … shape the economic landscape over the coming decades”]. Trillions of dollars are already being reallocated from sectors hurt by climate change to sectors that profit from it: the market rewards resilient business models and punishes vulnerable ones [Bloomberg, The Climate Economy Outlook, 2025].

+7 ppper year — outperformance of the S&P 500 by ‘Prepare & Repair’ companies over the past 3 years[Bloomberg, 2025]
+8.8 ppper year — outperformance by ‘clean’ leaders over their ‘dirty’ competitors (steel, cement, aviation and oil and gas)[Bloomberg, 2025]
Five ‘climate alpha’ clusters
Beneficiary sectorDriverKey metrics
AI infrastructure
ABB, Schneider Electric, Delta
Rising data-centre energy consumption due to AI → demand for power and cooling solutionsElectricity demand for AI and industry will grow by ≈3% a year through 2030 (up from 0.5%); 36 «AI Enablers» outperformed the global IT index S&P 1200 by 11 pp over 3 years and by 17 pp over 5 years
HVAC — air conditioning
Johnson Controls, Trane, Carrier
Record temperatures → demand for air conditioning and service contractsSector revenue is projected to rise from $70.9 billion (2024) to $94.8 billion by 2030 (≈+5% CAGR)
Prepare & Repair
Jacobs, Stantec, equipment hire, DIY retail
Spending on disaster preparedness and recovery; vulnerability audits; new reporting standardsThe 110-component index outperformed the S&P 500 by 4.5 pp over one year and by 9–12 pp over horizons of 3–10 years
Engineering and construction
Strabag, AtkinsRéalis, Larsen & Toubro
Recovery programmes; flood-control projectsOrders for flood control and infrastructure reconstruction (Austria, Switzerland, Poland, Australia and Brazil) support revenue
Insurance brokers
Arthur J. Gallagher, Aon
Rising insurance premiums due to climate risksThe main beneficiaries of rising risks are not insurers (which bear the losses) but brokers (which earn commission as turnover rises); they outperform the S&P 500

The Bloomberg ‘Prepare & Repair’ Index (BPRAET) brings together companies that benefit in two areas: ‘preparedness’ (adaptation — building products, risk management, consulting and storage) and ‘disaster recovery’ (HVAC, grid equipment, environmental services, insurance, engineering and emergency response). The ‘recovery economy’ has systematically outperformed the broad market over 3-, 5- and 10-year horizons [Bloomberg, 2025].

Context · water as infrastructureWater is an underappreciated driver of EU growth: water infrastructure faces an investment gap of hundreds of billions of euros, while inaction is already costing tens of billions a year. Key ‘industries of the future’ — semiconductors, data centres, ‘green’ hydrogen and batteries — are extremely water-intensive, and cannot grow unless water scarcity is addressed [WSP, Socio-economic study on the value of the EU investing in water].

Investor takeaway

Climate risks are creating durable tailwinds for five clusters that are delivering faster revenue growth and/or excess returns relative to the market. This is the core of the ‘climate alpha’ investment thesis — repricing cuts both ways (see Part VIII).

Final slide

Call to action

Every additional fraction of a degree of warming increases climate risks [IPCC AR6 SYR, 2023IPCC AR6 Synthesis Report“Every increment of global warming will intensify multiple and concurrent hazards ... Risks and projected adverse impacts and related losses and damages from climate change escalate with every increment of global warming”Web]. Every action matters — whether it helps or harms the climate. Knowledge and practices spread through example, multiplying their impact.

11.01 Personal Responsibility and a Realistic Perspective

The need for urgent action and radical decisions

Global institutions are not yet managing the crisis effectively. Many politicians, meanwhile, have little incentive to adopt radical measures: voters dislike them, and governments worldwide have deep ties to the fossil-fuel industry and industrial agriculture. Moreover, no one bears real responsibility for the future.

Businesses and society also often focus on short-term gains or pay too little attention to the problem, relying on governments — creating a vicious circle. Yet when institutions fail, private initiative becomes essential at a systemic level.

Even if everyone begins the transition to clean energy and sustainable agriculture and industry today, serious challenges will still lie ahead. Postponing change until tomorrow or waiting for others to start tackling the problem means making the task virtually impossible.

Radical change is needed now — today, without delay. The later these changes take place and the more compromises are made, the greater the hardship and danger that await us and our children in the coming decades.

11.02 Systemic Solutions

Comprehensive Solution

Clean Energy Cities (Open-Source Franchise)

Modern challenges demand a radical restructuring of core infrastructure and a rethinking of our very way of life. We invite specialists in relevant fields, engineers, and scientists from around the world to join forces on a nonprofit basis to develop initiatives such as “Clean Energy Cities” (CEC).

CEC is a global open-source project comprising a comprehensive set of operating protocols, principles, and specific technological solutions for creating a fundamentally new, sustainable living environment.

Cities account for approximately 70% of global greenhouse gas emissions and 67% of primary energy consumption; up to 70% of all food produced globally is destined for consumption in cities [IPCC AR6 WGIII, 2022IPCC AR6 WGIII — Summary for Policymakers“In 2020, urban emissions were estimated to be 29 GtCO2-eq (67–72% of the global share).”Web; UN-Habitat, 2024Urban Content of NDCs: 2024 Report“Cities are responsible for approximately 67 per cent of global primary energy consumption and 70 per cent of global greenhouse gas emissions.”Web; FAOFive ways to make cities healthier and more sustainable“People in urban areas consume up to 70 percent of global food supply.”Web]. However, experience shows that efforts to transform existing cities often encounter critical systemic barriers, making the process slower and more expensive than building from scratch. Moreover, maximum efficiency can be achieved only in new settlements whose architecture is designed from the outset around sustainable development goals. At the same time, many advanced solutions tested in such cities can subsequently serve as a foundation for modernizing traditional settlements.

The project’s objective is to develop an economically viable, open “franchise” of autonomous settlements with a closed-loop life-support system. The model will then be continuously scaled and refined through the adoption of innovations, in-depth analytics based on digital twins, and the open exchange of best practices among all members of the network.

Modular Design and Adaptability

To ensure flexible scaling and applicability across a wide variety of climatic conditions, we propose developing individual core modules of the system. These function as modular building blocks, allowing them to be combined in ways that account for the specific characteristics of particular regions, local needs, and available resources.

Basic Standards for the New Living Environment

The technical solutions incorporated into CEC should become a new standard for modern living and a benchmark for the transformation of megacities:

  1. Building Energy Efficiency: Deep integration of passive architecture principles.
  2. Energy Autonomy: Clean distributed and combined power generation paired with scalable energy storage systems.
  3. Local Automated Agricultural Production: A transition to sustainable agriculture without pesticides or toxic chemicals, with closed-loop water use and an emphasis on plant-based diets.
  4. Deep Multistage Water Filtration: Barrier protection for drinking-water supply systems and the agricultural sector against “forever chemicals” (PFAS), microplastics, and industrial pollutants.
  5. Eco-Friendly and Sustainable Materials.
  6. Sustainable Behavior Model (sustainable humans): A deliberate rejection of overconsumption, a radical reduction in the share of animal-derived products and ultra-processed foods, as well as a shift toward a preventive approach to health, long-term planning, and responsibility to future generations.
Response to Global Threats

Global adoption of this model will largely resolve the following issues:

  • Climate change;
  • The destruction of ecosystems and the rapid loss of biodiversity;
  • Widespread environmental pollution;
  • The degradation of freshwater sources and the risks of “Day Zero”;
  • The use of biochemical toxins in the production of food and materials;
  • Critical risks associated with food-supply dependence, including vulnerability to disruptions in global logistics chains or the world’s breadbasket regions;
  • Risks associated with the destruction of critical infrastructure during hostilities and natural disasters.

A natural outcome of implementing these standards will be not only environmental protection and the mitigation of climate risks, but also a substantial increase in life expectancy and quality of life. This outcome will be achieved by eliminating systemic toxic factors from which reliable protection is virtually impossible today, even in the most exclusive districts of traditional megacities.

Mechanics of Global Transformation

Many of the proposed technological solutions already exist and often prove more advantageous even from an economic standpoint, especially when used in environments designed around them from the outset. For example, solar panels can meet a significantly larger share of energy demand when installed on energy-efficient buildings designed according to passive architecture principles.

If the existing urban network were progressively replaced or modernized according to these standards, these crises would be largely resolved.

A potentially effective path to this goal is to initiate a natural large-scale movement of people. As traditional cities become increasingly vulnerable and dangerous, while environmental awareness and remote work become more widespread, healthy, autonomous, and safe Clean Energy Cities could become natural magnets for many people.

A brief overview of the other proposed initiatives can be found here. Their detailed descriptions will be provided in subsequent materials. We are also currently developing a new socioeconomic model, because effectively addressing global challenges extends beyond the material and technical domain and requires a comprehensive rethinking of every sphere of social life.

11.03 Practical Steps for Everyone

What can be done right now?

Investors, businesses and individuals need to act on two equally important fronts: reducing pressure on the climate (mitigation) and preparing for inevitable changes (adaptation). Hopes of a mild scenario are not being borne out — the world is heading towards a more extreme future.


Mitigation: reducing pressure on the climate

These steps address the root cause of warming by reducing greenhouse gas emissions.

  • Portfolio and asset decarbonisation. A shift to zero-carbon energy (solar, wind and other forms of clean energy) wherever possible. Phasing out fossil fuels (coal, gas and oil) — the primary cause of climate change.
  • Energy efficiency. Adopting green building standards, reducing heat loss and electrifying transport and household energy use.
  • Dietary changes. Reducing consumption of red and processed meat. Agriculture is the second-largest driver of climate change and the leading cause of biodiversity loss.
  • Sustainable consumption. Choosing products from companies that demonstrate genuine environmental responsibility (sustainability — developing their businesses without harming future generations), and refusing to support those whose activities directly harm the environment.

Adaptation: preparing for shocks

The impacts will intensify. It is vital to protect lives and capital.

  • Climate stress-testing of assets. Auditing real estate and businesses for vulnerability to extreme heat, flooding, drought and fire. Taking account of the fact that historical norms are becoming unreliable.
  • Investment in self-sufficiency. Independent energy supply systems (solar panels, wind turbines and storage systems), water supply systems (rainwater harvesting and treatment), local food production and other solutions.
  • Relocation and site selection. Avoiding asset development in vulnerable areas (southern countries, regions facing critical water stress, fire-prone forests, areas subject to recurrent flooding, and coastlines). Seeking out climate havens.
  • Accounting for new risk zones. Extreme events are shifting into areas historically considered safe (areas that previously did not flood or burn and were not exposed to hurricanes). Official zoning maps (for example, those produced by local authorities or emergency management agencies) are based on past statistics and often fail to keep pace with these new threats.
  • Supply-chain diversification. For businesses, avoiding dependence on a single supplier in regions exposed to climate shocks (particularly in the agro-industrial sector and logistics).

Actions spanning mitigation and adaptation

These steps are equally important for preventing catastrophe and mitigating its impacts.

Investor checklist.
Every asset should be assessed against two questions:
  • 1. How does this asset affect the climate? (Carbon footprint, direct and indirect greenhouse gas emissions, and harm to the environment and biodiversity).
  • 2. How does the climate affect this asset? (Physical risk: heat, water scarcity, fires and supply-chain disruption; repricing; transition risk: taxes on GHG emissions, carbon allowances and reputational risk).

Network effect

Take the initiative and spread the word. The wider public does not yet grasp the full scale and severity of the impacts of climate change. Your actions and personal example have a powerful network effect — this is how systemic change happens.



This report is continuously updated

The report is continuously revised as new data and feedback become available. Our goal is to maintain a coherent, up-to-date picture of the world, rather than produce a document that quickly becomes outdated. We invite specialists to join this initiative as part of the IEvoH .

Last updated

Change log

  1. Data from Bevacqua et al., Moderate global warming does not rule out extreme global climate outcomes (Nature, 2026), were added to Map → Food, Bad News → Impacts could be worse than expected, Wildfires → Future projections, and Floods → Future projections.

  2. Data from Reuters, BBC, The Straits Times, DutchNews, EEA/JRC, and viadonau on the Danube were added to Map: Logistics Chains and Energy.

  3. Material from the IEvoH White Paper was added to Solution → Comprehensive Solution.

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