Intergovernmental Panel on Climate Change SSP-RCP scenarios
The IPCC’s sixth Assessment Report (AR6) explores five emissions scenarios.
The IPCC’s sixth Assessment Report (AR6) explores five emissions scenarios.
The IPCC began its sixth assessment reporting cycle (AR6) in 2021. The AR6 assessment reports use SSP-RCP (‘SSPX-Y’) scenarios based on the Shared Socio-economic Pathways (SSPs), and partly informed by the Representative Concentration Pathways (RCPs) scenarios of AR5.
Read the IPCC’s sixth assessment (AR6) reports, including the summary for policymakers
The set of SSPs is described in Chapter 1 of the IPCC’s AR6 Working Group I report, Climate Change 2021: The Physical Science Basis. Chapter 4 describes the assumptions associated with each of the SSP-RCP scenarios.
The chapter includes figures comparing the differences between each scenario, such as:
The IPCC’s working group I (WGI) Interactive atlas is an online tool that allows users to explore projected climate change information underpinning each of the SSP-RCP scenarios.
The AR6 scenario explorer and database presents the dataset of quantitative, model-based pathways related to the mitigation of climate change which underpin the Sixth Assessment Report (AR6) of IPCC Working Group III.
The Intergovernmental Panel on Climate Change (IPCC) is the international body tasked with assessing the science of climate change.
Since 1988, the IPCC has informed policy makers on:
The IPCC released its Fifth Assessment Report (AR5) [Ipcc website] in 2014. The Fifth Assessment Report explores five different Representative Concentration Pathways (RCPs). Each RCP corresponds with a level of radiative forcing (and degree of global warming) by 2100.
The IPCC released its latest Sixth Assessment Report (AR6) [Ipcc website] in 2021. The Sixth Assessment Report explores five different Shared Socio-economic Pathways (SSPs) combined with Representative Concentration Pathways (RCPs). These AR6 scenarios are referred to as the ‘SSP-RCP’ scenarios (or the ‘SSPX-Y’ scenarios).
Read more about the history of the IPCC scenarios [Ipcc website] – including the SSPs and RCPs – in Chapter 1 of the Working Group I (WGI) Sixth Assessment Report (AR6).
The SSP-RCP scenarios (sometimes referred to as the ‘SSPX-Y scenarios’) combine the baseline SSPs with Representative Concentration Pathways (RCP) scenarios from the IPCC’s fifth assessment reporting period (AR5).
The SSP-RCP scenarios impose global warming targets on the baseline SSP scenarios using the radiative forcing levels of the RCP scenarios.
There are five SSP-RCP (‘SSPX-Y’) scenarios:
The first number ‘X’ in the SSPX-Y acronym refers to the baseline SSP scenario. The second number ‘Y’ refers to the RCP radiative forcing levels. For example, ‘SSP1-1.9’ is a scenario that combines SSP1 with 1.9 W m-2 radiative forcing in 2100 (RCP1.9).
The SSP-RCP (‘SSPX-Y’) scenarios are among the most commonly used global climate scenarios. The SSP-RCP scenarios combine baseline socio-economic narratives (the SSPs) with different emissions trajectories (based on the RCPs).
The SSP-RCP scenarios are useful building blocks (or scenarios ‘archetypes’) for creating scenarios, since they provide a global narrative, global emissions trajectory, and level of global warming upon which to build.
If you are developing scenarios with a broad focus, you may find it useful to align some, or all, of your scenarios with an equivalent IPCC SSP-RCP scenario. This will help create the structure of your scenarios by painting a picture of what is happening at a global scale.
NIWA is a crown research entity that has previously conducted modelling to downscale the IPCC AR5 data (2014) to the New Zealand scale.
NIWA will also be downscaling the IPCC’s AR6 data (2021) to the New Zealand scale. ‘Downscaling’ involves deriving local climate information from a larger scale model. The downscaled AR6 data for New Zealand is due for publication in 2024.
Read more about Climate data for Aoteaora New Zealand (based on the IPCC Fifth and Sixth Assessment Report scenarios).
The SSP-RCP scenarios incorporate assumptions about future socioeconomic developments, such as population growth, economic trends, and technological advancements.
The SSP-RCP scenarios assume a certain level of global cooperation and implementation of climate policies. Real-world political and societal dynamics may deviate from these assumptions, affecting the feasibility of mitigation and adaptation measures.
Other limitations of the SSP-RCP scenarios include:
The treatment of potential tipping points [Global Tipping Points website] and abrupt climate changes within the SSP-RCP scenarios is an area of ongoing research and uncertainty. Some critics argue that these scenarios may not fully account for the risks associated with tipping points.
Read more about climate tipping points in the What Planet Are We On? article pages 27-30 [Institute and Faculty of Actuaries website]
For more on the limitations of existing climate scenarios, including the IPCC scenarios, see the University of Exeter report Emperor’s New Climate Scenarios – a warning for financial services [Institute and Faculty of Actuaries website]
There are five SSP-RCP (‘SSPX-Y’) scenarios, each with a different set of narrative assumptions and emissions trajectories.
The baseline SSP scenarios provide descriptions of how the future may develop, based on a coherent and internally consistent set of assumptions about key driving forces (e.g., rate of technological change) and relationships. The RCP scenario components correspond to the level of radiative forcing at 2100.
The SSP-RCP scenarios drive climate model projections of changes in the climate system. Projections account for solar activity and background forcing from volcanoes.
Results over the 21st century are provided for the near term (2021–2040), mid-term (2041–2060), and long term (2081–2100) relative to 1850–1900 (unless otherwise stated).
Near term, 2021-2040 | Mid-term, 2041-2060 | Long-term, 2081-2100 | ||||
Scenario |
Best estimate (ºC)* |
Very likely range (ºC)* |
Best estimate (ºC)* |
Very likely range (ºC)* |
Best estimate (ºC)* |
Very likely range (ºC)* |
SSP1-1.9 | 1.5 | 1.2 to 1.7 | 1.6 | 1.2 to 2.0 | 1.4 | 1.0 to 1.8 |
SSP1-2.6 | 1.5 | 1.2 to 1.8 | 1.7 | 1.3 to 2.2 | 1.8 | 1.3 to 2.4 |
SSP2-4.5 | 1.5 | 1.2 to 1.8 | 2.0 | 1.6 to 2.5 | 2.7 | 2.1 to 3.5 |
SSP3-7.0 | 1.5 | 1.2 to 1.8 | 2.1 | 1.7 to 2.6 | 3.6 | 2.8 to 4.6 |
SSP5-8.5 | 1.6 | 1.3 to 1.9 | 2.4 | 1.9 to 3.0 | 4.4 | 3.3 to 5.7 |
*Temperature differences relative to the average global surface temperature of the period 1850-1900 are reported in ºC.
The Socio-economic Pathways (SSPs) provide baseline narratives. The SSPs form part of the basis for modelling the combined SSP-RCP scenarios.
The world shifts gradually, but pervasively, toward a more sustainable path, emphasising more inclusive development that respects perceived environmental boundaries.
The world follows a path in which social, economic, and technological trends do not shift markedly from historical patterns. Development and income growth proceeds unevenly, with some countries making relatively good progress while others fall short of expectations.
A resurgent nationalism, concerns about competitiveness and security, and regional conflicts push countries to increasingly focus on domestic or, at most, regional issues. Policies shift over time to become increasingly oriented toward national and regional security issues.
Highly unequal investments in human capital, combined with increasing disparities in economic opportunity and political power, lead to increasing inequalities and stratification both across and within countries.
Over time, a gap widens between an internationally connected society that contributes to knowledge- and capital-intensive sectors of the global economy, and a fragmented collection of lower-income, poorly educated societies that work in a labour-intensive, low-tech economy.
This world places increasing faith in competitive markets, innovation, and participatory societies to produce rapid technological progress and development of human capital as the path to sustainable development.
These summaries for the SSP baseline narratives are adapted from a Riahi et al. 2017 article in Global Environmental Change [ScienceDirect website].
Read more about the SSPs in the IPCC’s Sixth Assessment Report (AR6) [Ipcc website].
The RCP components of the SSP-RCP scenarios impose a level of radiative forcing in 2100, which corresponds with a related level of global warming.
RCP |
Radiative forcing level |
Description |
RCP1.9 | 2.6 W m-2 radiative forcing in 2100 | Very stringent mitigation scenario |
RCP2.6 | 2.6 W m-2 radiative forcing in 2100 | “Stringent mitigation” scenario |
RCP4.5 | 4.5 W m-2 radiative forcing in 2100 | Intermediate scenario |
RCP6.0 | 6.0 W m-2 radiative forcing in 2100 | Intermediate scenario (higher warming than RCP4.5) |
RCP8.5 | 8.5 W m-2 radiative forcing in 2100 | Very high warming scenario |
Read more about the RCPs in the IPCC’s Fifth Assessment Report (AR5) [Ipcc website]