Planetary Risk, Priced
The Earth Security Dashboard
Beta 0.6

The dashboard tracks how planetary stress is being priced into capital markets. It monitors the repricing of environmental volatility into premiums, spreads, asset valuations and capital flows, shaping a direction for global resilience capital.

Q1 2026
This beta edition is designed to generate early institutional feedback in the development of frameworks, pricing signals, analyses and applications.
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Signal Overview

Signal Overview

Live readings across all five repricing channels. Scores represent each signal's position within its historical range (0 = historical low, 100 = historical high). Dot colour follows absolute severity against threshold.

Panel A
Insurance Stress
Elevated
Insured Catastrophe Losses
43 /100
Uninsured Fiscal Exposure
51 /100
Insurance-Linked Securities
99 /100
Panel B
Sovereign Resilience
Elevated
Sovereign Resilience Divide
77 /100
Sovereign Green Bond Market
70 /100
Panel C
Trade Friction
Elevated
Bulk Freight Costs
30 /100
Supply Chain Stress
11 /100
Panel D
Asset Valuation
Acute
Power Grid Vulnerability
81 /100
Water Asset Discount
30 /100
Panel E
Resource Volatility
Elevated
Global Food Price Pressure
47 /100
Commodity Instability
40 /100

Scores: position within historical range (0–100) · Colour: bar fill severity classification · Deep-dive data below ↓

Panel Deep Dive
A
Panel A · Insurance & Risk Transfer
Insurance Stress Monitor
Elevated
Insurance markets reprice physical climate risk before equity or credit markets respond, with pricing pressure transmitting into land, infrastructure, and municipal bond valuations among others. This makes premium inflation, protection gaps, and withdrawal patterns the earliest cross-asset signal of climate-driven financial stress.
Global Insured Catastrophe Losses — Annual Total (USD)
$107B
USD billion
−24% vs. 2024
Data: Full Year 2025
2020 ($81B)2024 high ($141B)
Global insured catastrophe losses reached $107 billion in 2025, a 24% decline from the 2024 record of $141 billion, below the $111 billion ten-year average. Despite this below-average year, Sigma notes this was a favourable draw, not a reduction in risk, the long-term growth trend implies a 2026 loss of $148 billion. The current decline from the previous year is compositional rather than indicative of reduced physical risk: 2025’s loss total was heavily shaped by the concentration of major events in deeply insured US markets, masking the continued expansion of uninsured exposure in emerging market geographies. The long-run trajectory is unambiguously upward, driven by three compounding forces: the accumulation of insured assets in climate-exposed zones, the increasing frequency of secondary perils such as convective storms and wildfires, and the repricing of primary perils as insurers update return-period assumptions in response to observed loss experience.
Source: Swiss Re Sigma · Annual
Natural Catastrophe Protection Gap — Uninsured Share of Total Economic Losses
51.4%
% uninsured
Structurally narrowing
Data: Full Year 2025
0%100%
The protection gap, meaning the share of total economic losses that goes uninsured, indicates how much climate damage falls on governments, households, and public balance sheets rather than private risk capital, with a widening gap signalling growing fiscal exposure at the municipal and sovereign level that does not yet appear in credit spreads. While the protection gap narrowed slightly in 2025 to 51.4% this was due to the share of insured losses reaching a record high – given the high concentration of 2025’s disasters (like the LA wildfires) occurred in well-insured U.S. markets.
Source: Swiss Re Sigma · Annual · Derived: (Total economic losses − Insured losses) ÷ Total economic losses
Catastrophe Bond Issuance Volume — Annual Total (USD)
$25.0B
USD million (rolling)
Near-record
Data: Rolling 12m to Mar 2026
(~$5.2B rolling, Oct 2019)($25.2B rolling, Dec 2025)
Catastrophe bond issuance reached $25.0 billion on a rolling 12-month basis to March 2026, near the all-time record and +23.9% above the prior year (rolling 12-month), confirming that the transfer of catastrophe risk from insurers to capital markets has crossed a structural threshold driven by an insurance industry absorbing some of its costliest loss years on record. The concentration of this issuance, over 93% tied to North American perils, reveals a profound geographic mismatch: capital markets have developed institutional appetite for packaging and pricing catastrophe risk, but that sophistication has not yet been deployed at scale in the coastal and climate-vulnerable emerging market sovereigns where physical risk is growing fastest and adaptation finance is most scarce.
Source: Artemis Deal Directory · Quarterly
B
Panel B · Sovereign Risk & Cost of Capital
Sovereign Resilience Spread Monitor
Elevated
Sovereign debt markets are where climate vulnerability is translated directly into borrowing costs. As climate shocks compress fiscal space and raise emergency expenditure, spreads widen, repricing the cost of capital for the most exposed governments. This structural repricing positions sovereign green bond issuances and debt-swaps for climate to increasingly command resilience premiums.
Vulnerability Gap Score – High vs. Low Resilience Sovereigns
0.268
Score gap (0–1)
Widening since 2014
Data: 2023 (latest available)
0 (no divergence)0.35
The vulnerability gap score measures the structural divergence in climate resilience between the world’s most and least prepared sovereigns, capturing exposure, sensitivity, and adaptive capacity across food, water, health, infrastructure, and human habitat in a single normalised score. At 0.268, the gap represents nearly the full span of meaningful difference in how countries survive climate stress, having remained structurally elevated since 2010 with no material sign of closing. It confirms that the distance between the most resilient and most vulnerable sovereign cohorts is not a transitional condition but a deepening structural feature of the global economy. The IMF has established that a one percentage point increase in climate vulnerability corresponds to approximately 15.5 basis points of additional sovereign risk premium independent of conventional fiscal metrics, meaning the 0.268 gap implies a spread differential of over 400 basis points between the top and bottom resilience quartiles that conventional credit analysis systematically underprices. The implication is that sovereign green and resilience bonds issued by bottom-quartile sovereigns carry an embedded and growing climate risk premium that, if properly structured and disclosed, represents both a genuine yield opportunity for investors and a mechanism for directing concessional and blended capital toward the adaptation investments that are the only credible path to narrowing the gap itself.
Source: ND-GAIN Country Index, University of Notre Dame · Annual
Sovereign Green, Social & Sustainability Bond Issuance — Annual Volume (USD)
$124.7B
USD billion
−25.6% YoY
Data: Full Year 2025
2019 baseline ($25B)2024 record ($167.4B)
Sovereign green, social, and sustainability bond issuance measures the volume of labelled debt issued by national governments to finance climate adaptation, mitigation, and social resilience programmes, the most direct signal of how sovereign borrowers are mobilising capital markets to fund the transition. At $124.7 billion in 2025, issuance declined 25.6% from the 2024 peak, driven primarily by US-induced ESG sentiment reversal, but the market has grown fivefold since 2019, confirming that sovereign appetite for sustainability finance has fundamentally reset to a structurally higher base rather than retreating. At roughly 25% of the estimated $500 billion annual run-rate required to meet Paris-aligned adaptation financing needs, the gap between sovereign ambition and sovereign action remains the defining financing shortfall of the decade, and the most consequential opportunity in the resilience capital universe. As the vulnerability gap widens and sovereign climate risk premiums reprice, the incentive for bottom-quartile sovereigns to issue resilience-linked instruments at credible terms will intensify.
Source: Climate Bonds Initiative State of the Market · Annual
C
Panel C · Trade & Logistics Friction
Trade & Logistics Friction Monitor
Elevated
Climate disruption, geopolitical fragmentation, and tariff uncertainty are converging on global trade and logistics simultaneously, transmitting into freight rates, input costs, and corporate margins through the same physical infrastructure, making trade friction a compounding real-time signal for resilience capital deployment costs and sovereign fiscal capacity.
Baltic Dry Index (BDI) — Dry Bulk Freight Rate Benchmark
1,955
Index points
+20.0% above post-2022 mean (1,629)
Data: Q1 2026 avg
series low (393, May 2020)5-yr high (5,650)
A Q1 2026 BDI averaging 1,955, above the post-2022 mean despite the seasonally weakest quarter, signals that global bulk commodity demand is holding firm under geopolitical and tariff uncertainty. For climate-vulnerable sovereign borrowers and green transition capital deployment, this sustained freight floor means input cost inflation is structural rather than transient: construction materials, food imports, and energy inputs are all arriving at persistently elevated landed costs in the markets where fiscal adaptation budgets are thinnest.
Source: Baltic Exchange · Daily
Global Supply Chain Pressure Index (GSCPI) — Standard Deviations from Historical Average
+0.49σ
Std. deviations (σ)
Building from 2023 low
Data: Feb 2026
0σ avg2022 peak (+4.49σ)
Global supply chain pressures returned to above-average territory in Q1 2026, with the GSCPI reaching +0.49σ in February, a signal that the two-year window of unusually benign supply conditions has closed. This renewal of supply chain pressure is driven by a combination of new geopolitical conflicts, structural environmental issues affecting major shipping routes, and high levels of trade uncertainty. For resilience capital, this shift is structurally significant: the cost environment in which most sustainable infrastructure project financial models were built, characterised by sub-zero GSCPI readings and freight rates near multi-year lows, no longer exists, and IRR assumptions calibrated to that period are now subject to upward input cost pressure across construction materials, logistics, and equipment procurement in target geographies.
Source: NY Federal Reserve Bank · Monthly
D
Panel D · Asset Valuation & Capital Rotation
Asset Resilience Valuation Monitor
Acute
Resilient assets are beginning to command measurable premiums over climate-exposed equivalents, and to trade at a discount when that resilience is absent. This divergence, visible across listed infrastructure, grid vulnerability, and adaptation-linked issuances, is the leading indicator of structural capital rotation toward physical climate security.
Climate-Driven Grid Stress Ratio — US Annual (Dimensionless)
5.03
ratio (times worse)
+70% vs 2023, highest on record
Data: Full Year 2024
1.0 (no stress)6.0 (extreme)
The Climate-Driven Grid Stress Ratio measures how much worse the US electricity grid performs during major climate events relative to normal operating conditions, expressed as a ratio of outage duration with major event disturbances to outage duration without them. A reading of 5.03 means that when a qualifying climate event strikes, customers experience grid outages more than five times longer than baseline. The 2024 reading is the highest in the ten-year series and represents a 70% deterioration from 2023’s 2.96, confirming that the trend is not a gradual drift but an accelerating structural breakdown in the resilience of critical energy infrastructure under climate stress. The ratio captures a compounding vulnerability: as climate events intensify in frequency and severity, grid infrastructure built to historical weather tolerances is increasingly exposed, while the cost of hardening that infrastructure, undergrounding, vegetation management, substation flood-proofing, distributed generation, remains largely unpriced in utility equity valuations and municipal bond spreads. For resilience capital, the signal has direct implications across multiple asset classes: utility equity investors face unmodelled capex exposure as regulators begin mandating climate-hardening investment; infrastructure debt allocators holding transmission and distribution assets in climate-exposed geographies face deteriorating coverage ratios as storm-related restoration costs compound; and sovereign and sub-sovereign issuers in regions with high grid stress exposure face growing fiscal pressure from emergency response, economic disruption, and the political cost of repeated outage events.
Source: EIA Electric Power Annual, Table 11.1 · Annual
S&P Global Water Index vs. S&P Global Infrastructure Index — Rolling 1-Year Return Differential
−10.0%
Return differential
Water underperforming Q1 2026
Data: 31 Mar 2026
Max underperformance (−25.6%, Aug 2022)Max outperformance (+27.0%, Aug 2021)
The −10.0% return differential between global water equities and broad infrastructure in Q1 2026 reflects a confluence of temporary market forces, interest rate sensitivity hitting long-duration water utility valuations harder than energy and transport infrastructure, and ESG sentiment retreat reducing the narrative premium on water-specific exposure. This signal suggests that equity markets are temporarily discounting a theme whose physical urgency is accelerating, not diminishing, and an unpriced rating catalyst is building in the form of AI and data centre water demand that has not yet found its way into listed valuations. For resilience capital allocators, the practical implication is a valuation opportunity window in unlisted water infrastructure, when listed water equities underperform, implied discount rates on private water infrastructure assets rise, meaning project-level entry multiples become more attractive precisely when the long-run investment case is most compelling.
Source: S&P Dow Jones Indices · Daily
E
Panel E · Resource Volatility
Resource Volatility Monitor
Elevated
The convergence of climate- and geopolitically-driven disruptions that lead to commodity volatility and elevated food prices transmit supply disruptions directly into sovereign fiscal positions, corporate earnings, and inflation dynamics, amplifying stress across every other panel in this dashboard and compressing the adaptation budgets of the economies most exposed to physical climate risk.
FAO Food Price Index — Nominal Composite (Cereals, Oils, Sugar, Dairy, Meat)
125.3
Index (2014-16=100)
−1.0% vs. Feb 2025
Data: Feb 2026
2015–19 avg (94.73)2022 peak (160.2)
The FAO Food Price Index reading of 125.3 in February 2026 means internationally traded food commodities cost 25.3% more than the 2014–16 baseline, and critically, despite the retreat from the 2022 peak, prices are consolidating 32% above the pre-pandemic norm of 94.73, confirming a structural reset in the global food price floor rather than a cyclical correction. The February uptick, driven simultaneously by frost-damaged wheat harvests in Europe and the US, Black Sea logistical disruption, and palm oil supply tightening in Southeast Asia, illustrates a compounded climate-geopolitical transmission mechanism. The score suggests a permanent fiscal drag on the sovereign cohort most exposed to physical climate risk, food-importing, low-resilience economies in Africa, South Asia, and Southeast Asia where every weather shock now transmits into import costs, current account pressure, and eroded adaptation budgets.
Source: FAO Food Price Index · Monthly
Agricultural Commodity Price Volatility Composite — Annualised Rolling (Derived Metric)
16.7%
Annualised volatility (%)
+1.1pp vs. 2019–22 avg
Data: Feb 2026
2019 avg (10.97%)2022 peak (25.3%)
Agricultural commodity price volatility measures how unpredictably food commodity prices are moving, expressed as an annualised standard deviation of monthly price changes across cereals, oils, sugar, dairy, and meat. At 16.7% in February 2026, the composite sits marginally above the 2019–22 mean of 15.6%, signalling that markets have stabilised from the 2022 crisis peak of 25.3% but have not returned to the low-volatility regime that preceded it. The surface calm masks compounding forward risks: winterkill damage to Black Sea and European wheat crops, drought stress in Argentine breadbaskets, and a sharp rise in natural gas prices transmitting into nitrogen fertiliser input costs ahead of the Northern Hemisphere’s spring planting, a sequence that could spike volatility sharply from its current floor. For resilience capital, sustained above-average agricultural volatility is a fiscal risk multiplier at every scale, compressing household purchasing power and government food subsidy budgets in food-importing sovereigns, while simultaneously disrupting corporate supply chain planning, agribusiness earnings, and the inflation outlook for central banks managing the cost-of-living transmission in advanced economies.
Source: World Bank Pink Sheet · Monthly · Derived calculation
Cross-Panel Relationships

Cross-Panel Relationships

The five panels of the Dashboard reflect an interconnected system. The four structural transmission relationships below explain how the repricing of planetary risk propagates across asset classes.

01
The Compounding Cycle
Insurance withdrawal from a high-risk region removes the financial floor from property values (Panel D), erodes municipal tax bases, widens sub-sovereign spreads (Panel B), and increases the fiscal cost of infrastructure resilience, which delays adaptation and increases future insurance loss exposure (Panel A). The Dashboard maps these second- and third-order effects as compounding risk clusters.
02
Leading vs. Lagging Signals
The five domains operate on different time horizons. Insurance pricing (Panel A) and freight rates (Panel C) move first, within weeks to months of a stress event. Sovereign spread movements (Panel B) and resource price volatility (Panel E) respond within quarters. Asset valuation divergence (Panel D) unfolds over years. Reading the domains in sequence identifies where a repricing cycle is in its progression and which asset classes still have adjustment ahead of them.
03
Resilience Capital Formation Signal
Across the five domains, a parallel signal tracks the institutional formation of resilience-oriented capital, cat bond issuance (Panel A), sovereign green bond market depth (Panel B), and water infrastructure equity premiums (Panel D). When this formation signal strengthens across multiple panels simultaneously, it indicates that institutional capital is pricing Earth-system risk as a core investment variable across market segments.
04
Sovereign–Resource–Trade Nexus
The intersection of sovereign fiscal stress (Panel B), food price volatility (Panel E), and trade route disruption (Panel C) creates compounding sovereign refinancing risk, visible only when three panels are read together. Climate shocks that simultaneously reduce agricultural export capacity, disrupt logistics corridors, and compress fiscal space in the same geography place sovereigns under multi-channel pressure. The Horn of Africa, South Asia, and parts of Latin America currently sit at this triple intersection.
Biophysical Boundaries

Biophysical Boundaries

The indicators below track the upstream Earth-system conditions that drive repricing across the financial dashboard. Each is measured against a scientifically established security threshold. Where a boundary has been crossed or is under pressure, the financial signals in the panels above reflect downstream transmission of that stress. These are conditions, not forecasts. Update cadences range from monthly to annual; all sources are publicly available institutional datasets.

B1 · Atmosphere
Global Mean Surface Temperature Anomaly
+1.24 °C above pre-industrial −0.02°C YoY
Data: Feb 2026
Pre-industrial baseline (0°C)
1.5°C Paris limit
Approaching breach: 0.26°C below Paris threshold

Measures the increase in global average surface temperature relative to the 1850–1900 pre-industrial baseline, expressed as a 12-month rolling anomaly. Tracks atmospheric heat accumulation.
Security threshold: 1.5°C (Paris Agreement Article 2; Rockström et al. 2009 planetary boundaries). 2.0°C represents the outer agreed limit above which risk of self-reinforcing feedback loops increases materially.
Source: NASA GISS Surface Temperature Analysis (GISTEMP v4) · Monthly
B2 · Ocean System
Global Ocean Heat Content — Upper 2,000m
+33.3 ×10²² Joules vs. 1981–2010 mean +1.09 ZJ QoQ
Data: Q4 2025
1981–2010 mean (0 ZJ)
20 ZJ safety reference
Boundary exceeded: accelerating accumulation

Measures total heat energy stored in the top 2,000m of the global ocean relative to the 1981–2010 climatological mean. The ocean absorbs ~90% of excess atmospheric heat. OHC drives hurricane and cyclone intensification, thermal expansion sea level rise, and coral bleaching.
Security threshold: IPCC AR6 (2021) identifies sustained positive OHC anomaly above the 1981–2010 baseline as indicative of committed future warming and irreversible sea level rise. Continued accumulation locks in multi-decade insurance and sovereign fiscal exposure.
Source: NOAA NCEI Global Ocean Heat Content · Quarterly
B6 · Freshwater
Countries at or Above Freshwater Stress Threshold
38.6 % of sovereign nations Entrenched at 38.6%, no improvement since 2000
Data: 2022 (latest available)
0%100%
38.6% of nations in structural water stress, unchanged since 2000

Share of sovereign nations whose total annual freshwater withdrawal equals or exceeds 20% of available renewable freshwater resources. Persistent water stress at scale is a structural amplifier of food insecurity, sovereign fiscal fragility, and uninsurable physical risk.
Security threshold: FAO AQUASTAT / World Bank (SDG 6.4.2): freshwater withdrawal exceeding 20% of available renewable resources defines a country as water stressed at national scale, indicating structural supply pressure requiring adaptation investment at scale.
Source: FAO AQUASTAT via World Bank World Development Indicators · Annual (2022 latest)
B4 · Cryosphere
Arctic Sea Ice Extent — September Minimum
4.60 million km² +0.35M km² vs. 2024
Data: Sep 2025
0 km²6.22M km² average
26.0% below 1981–2010 average

Annual minimum sea ice area in the Arctic Ocean (September). Declining extent opens new shipping routes and resource extraction zones, amplifies polar warming via albedo loss, and intensifies mid-latitude extreme weather.
Security threshold: 1981–2010 satellite median (6.85M km²) as NSIDC baseline. First ice-free Arctic summer (<1M km²) is projected before 2050, a geopolitical and commercial threshold with direct implications for Arctic shipping routes and resource jurisdiction.
Source: NSIDC Sea Ice Index v3 · Annual (September minimum)
B5 · Atmosphere
Atmospheric CO₂ Concentration
429.35 ppm +2.26 ppm YoY
Data: Feb 2026
280 ppm pre-industrial500 ppm
350 ppm safe boundary
450 ppm / ~2°C
79.35 ppm above safe planetary boundary

Monthly mean atmospheric CO₂ at Mauna Loa Observatory, the longest continuous instrumental record (since 1958). CO₂ concentration is the master forcing variable driving climate risk.
Security threshold: 350 ppm (Rockström et al. 2009 planetary boundaries; adopted by major institutional investor frameworks). 450 ppm approximates the concentration associated with >2°C warming under IPCC AR6 scenarios.
Source: NOAA GML Mauna Loa Observatory (Keeling Curve) · Monthly