Calculate climate change

Calculates climate change analysis as a post-analysis action using the specified analysis result as a reference analysis.

This operation supports analysis based on a variety of RCP (Representative Concentration Pathway) scenarios and SSP (Shared Socioeconomic Pathways) scenarios that project the impact of greenhouse gas emissions based on diverse climate policies.

During processing, the Climate Change Model recalculates average annual loss (AAL) and EP metrics for portfolio and treaty levels.

RCP scenarios

RMS Climate Change Models provide a probabilistic view of a range of representative concentration pathways (RCPs). They model the effect of climate change on hurricanes in the North Atlantic and on windstorms and floods in Europe. The Climate Change Models cover the same geographical scope as the RMS reference models for these regions.

This operation supports modeling based on four RCP scenarios.

rcpScenarioDescription
2.6A pathway where radiative forcing peaks at approximately 3 W m-2 before 2100 and then declines to 2.6 W m-2.
4.5An intermediate stabilization pathway in which radiative forcing is stabilized at approximately 4.5 W m-2 and 6.0 W m-2 after 2100.
6.0An intermediate stabilization pathways in which radiative forcing is stabilized at approximately 4.5 W m-2 and 6.0 W m-2 after 2100.
8.5A high pathway for which radiative forcing reaches greater than 8.5 W m-2 by 2100 and continues to rise for some amount of time.

This operation supports RCP climate change analysis for reference analysis modeled using the following models:

ModelEngineSupported Versions
EUFL: Europe Inland FloodHD1.0 and later
EUWS: Europe WindstormDLMAny
EUWS: Europe WindstormHD1.0 and later
JPWS: Japan Typhoon and FloodHD2.0 and later
NAHU: North Atlantic HurricaneDLMAny
NAWF: North America WildfireHD1.0
NZFL: New Zealand Inland FloodHD1.0
USFL: US Inland FloodHD1.1 and later

SSP scenarios

This operation supports four scenarios (1-2.6, 2-4.5, 3-7.0, 5-8.5 ) that combine SSP scenarios (SSP1, SSP2, SSP3, SS5) and RCP scenarios (2.6, 4.5, 7.0, 8.5). Each scenario represents a unique set of socioeconomic and emission trajectories.

sspScenarioSSP ScenarioRCP Equivalent
1-2.6SSP1: Sustainability ("Taking the Green Road")2.6
2-4.5SSP2: "Middle of the Road"4.5
3-7.0SSP3: Regional Rivalry ("A Rocky Road")7.0
5-8.5SSP5: Fossil-fueled Development ("Taking the Highway")8.5

This operation supports SSP climate change analysis for reference analysis based on the following models:

ModelEngineSupported Versions
AUBF: Australia BushfireHD1.0
NAWF: North America WildfireHD2.0

Climate change model support

All Climate Change Model analyses, except for the North Atlantic Hurricane Models, are performed as a post-processing step on existing model results.

The reference analysis must be modeled using the following versions:

ModelRegionmodelRegionCodeperilCodesoftwareVersionCode
Australia Bushfire HD ModelAustraliaAUBFFRHDv1.0
Europe Inland Flood HD ModelsEuropeEUFLFLHDv2.1
Europe Windstorm HD ModelsEuropeEUWSWSHDv1.2
Europe Windstorm ModelsEuropeEUWSWSRL25, RL24, RL23, RL22, RL21, RL18.1, RL18
Japan Typhoon and Flood HD ModelJapanJPWSWSHDv2.1
New Zealand Inland Flood HD ModelNew ZealandNZFLFLHDv1.0
North America Wildfire HD ModelsNorth AmericaNAWFWFHDv1.0, HDv2.0
North Atlantic Hurricane ModelsNorth AtlanticNAHUWSRL25, RL24, RL23, RL22, RL21, RL18.1, RL18
US Inland Flood HD ModelUnited StatesUSFLFLHDv1.3

To learn more, see Climate Change Model Requirements and Features in Support Center.

🍊

Licensing

To calculate climate change analysis, you must license both the base models used in reference analysis and RMS Climate Change Models for all sub-regions in the original results.

Base models include Europe Inland Flood HD Models, Europe Windstorm Models, Japan Typhoon and Flood HD Model, North America Wildfire HD Model, North Atlantic Hurricane Models, US Inland Flood HD Model

🪰

Entitlements

RI-EXPOSUREIQRI-RISKMODELERRI-UNDERWRITEIQ
Headers
uuid
required
Defaults to xxxxxxxx-xxxx-xxxx-xxxx-xxxxxxxxxxxx

ID of resource group. To learn more, see Resource Groups

Path Params
int64
required
≥ 1

ID of reference analysis.

Reference analysis must be modeled using a model that supports climate change analysis. For a complete list, see Climate Change Model Requirements in Support Center.

Body Params
string
enum
required
Allowed:
string

Name of climate change analysis. Can be alphanumeric string.

string
enum
required

View depends on the base model used in reference analysis.

  • NAHU reference analyses support Combined - All Parameters or Frequency and Intensity Only
  • All other models support Default only.
Allowed:
int32
enum
required

ID of event rate scheme conditioned for climate change.

IDModelCodeEngine
1RMS 2011 Historical Event RatesUSFLHD
4RMS 2019 Historical Event RatesUSFLHD
6RMS v1.0 Default Rates (US)NAWFHD
7RMS v1.0 Default Rates (US+CA)NAWFHD
9RMS v2.0 Default RatesEUFLHD
14RMS v2.0 Stoch (Typhoon and Non-typhoon)JPWSHD
15RMS v2.0 Stoch (Typhoon)JPWSHD
16RMS v2.0 Stoch (Non-typhoon)JPWSHD
17RMS v1.0 Default RatesNZFLHD
18RMS 2011 Historical Rates (TC)USFLHD
19RMS 2019 Historical Rates (TC)USFLHD
21RMS 2021 Historical Event RatesUSFLHD
23RMS 2021 Historical Event Rates (TC)USFLHD
26RMS HDv1.0 Stoch Event Set (Default)EUWSHD
27RMS HDv1.0 Stoch Event Set (Unclustered)EUWSHD
35RMS 2023 Historical Event RatesUSFLHD
37RMS 2023 Historical Event Rates (TC)USFLHD
39RMS 2011 Historical Event Rates (Non-TC)USFLHD
40RMS 2023 Historical Event Rates (Non-TC)USFLHD
65RMS 2025 Historical Event RatesUSFLHD
66RMS 2025 Historical Event Rates (TC)USFLHD
67RMS 2025 Historical Event Rates (Non-TC)USFLHD
84RMS 2015 Stochastic Event RatesEUWSDLM
190RMS 2019 Historical Event RatesNAHUDLM
202RMS 2021 Historical Event RatesNAHUDLM
577RMS 2023 Historical Event RatesNAHUDLM
738RMS 2025 Historical Event RatesNAHUDLM
double
enum
required

RCP scenario. One of 2.6, 4.5, 6.0, or 8.5.

  • 2.6: A pathway where radiative forcing peaks at approximately 3 W m-2 before 2100 and then declines to 2.6 W m-2.
  • 4.5: An intermediate stabilization pathway in which radiative forcing is stabilized at approximately 4.5 W m-2 and 6.0 W m-2 after 2100.
  • 6.0: An intermediate stabilization pathways in which radiative forcing is stabilized at approximately 4.5 W m-2 and 6.0 W m-2 after 2100.
  • 8.5: A high pathway for which radiative forcing reaches greater than 8.5 W m-2 by 2100 and continues to rise for some amount of time.
Allowed:
int32
required

Snapshot year to include in RCP scenario-based analysis. A single five-year interval between 2020 and 2100, e.g. one of 2020, 2025, 2030, etc.

boolean

Indicates whether the climate change analysis includes RCP scenarios. If no rcpScenario or timeHorizon values are specified, set to false.

Responses

Language
Credentials
URL
LoadingLoading…
Response
Choose an example:
*/*
application/json