The Scenario Model Intercomparison Project (ScenarioMIP) for CMIP6
Open accessPublished version of a preprint
Abstract
Abstract. Projections of future climate change play a fundamental role in improving understanding of the climate system as well as characterizing societal risks and response options. The Scenario Model Intercomparison Project (ScenarioMIP) is the primary activity within Phase 6 of the Coupled Model Intercomparison Project (CMIP6) that will provide multi-model climate projections based on alternative scenarios of future emissions and land use changes produced with integrated assessment models. In this paper, we describe ScenarioMIP's objectives, experimental design, and its relation to other activities within CMIP6. The ScenarioMIP design is one component of a larger scenario process that aims to facilitate a wide range of integrated studies across the climate science, integrated assessment modeling, and impacts, adaptation, and vulnerability communities, and will form an important part of the evidence base in the forthcoming Intergovernmental Panel on Climate Change (IPCC) assessments. At the same time, it will provide the basis for investigating a number of targeted science and policy questions that are especially relevant to scenario-based analysis, including the role of specific forcings such as land use and aerosols, the effect of a peak and decline in forcing, the consequences of scenarios that limit warming to below 2 °C, the relative contributions to uncertainty from scenarios, climate models, and internal variability, and long-term climate system outcomes beyond the 21st century. To serve this wide range of scientific communities and address these questions, a design has been identified consisting of eight alternative 21st century scenarios plus one large initial condition ensemble and a set of long-term extensions, divided into two tiers defined by relative priority. Some of these scenarios will also provide a basis for variants planned to be run in other CMIP6-Endorsed MIPs to investigate questions related to specific forcings. Harmonized, spatially explicit emissions and land use scenarios generated with integrated assessment models will be provided to participating climate modeling groups by late 2016, with the climate model simulations run within the 2017–2018 time frame, and output from the climate model projections made available and analyses performed over the 2018–2020 period.
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Written from the paper’s full text.
TL;DR
ScenarioMIP is CMIP6’s primary scenario activity, providing multi-model climate projections driven by SSP-based emissions and land-use scenarios from integrated assessment models. It defines eight 21st-century scenarios plus a large initial-condition ensemble and long-term extensions, organized into two priority tiers.
Key findings
- The design comprises eight alternative 21st-century scenarios plus one large initial-condition ensemble and long-term extensions, split into Tier 1 (required) and Tier 2; Tier 1 includes SSP5-8.5, SSP3-7.0, SSP2-4.5, and SSP1-2.6, while Tier 2 adds SSP4-6.0, SSP4-3.4, SSP5-3.4-OS, and SSPa-b (around or below 2.0 W m⁻²).
- Forcing levels span updated RCPs (2.6, 4.5, 6.0, 8.5 W m⁻²) and gap scenarios (7.0, 3.4, below 2.6 W m⁻², overshoot); SSP1-2.6 is expected to produce 1.7 °C warming by 2100, and SSPa-b is designed to likely stay below 1.5 °C by 2100.
- Statistically significant local temperature differences over more than half the land surface require at least 0.3 °C global mean temperature separation, roughly equivalent to about 0.75 W m⁻² in an idealized 1 % yr⁻¹ CO₂ increase experiment; regional precipitation requires a much wider separation.
- Long-term extensions to 2300 include SSP5-8.5 extension equilibrating just above 12 W m⁻², SSP1-2.6 extension stabilizing around 2.0 W m⁻² and ~1.25 °C, and the overshoot extension peaking at ~2.4 °C and equilibrating at ~1.25 °C.
Methods
- Design/protocol paper: describes ScenarioMIP objectives, experimental design, and relation to other CMIP6 activities; scenarios are selected from SSP-based IAM marker scenarios, with harmonized spatially explicit emissions and land use to be provided to climate modeling groups by late 2016 and simulations run in 2017–2018.
- Experiments are concentration-driven for long-lived greenhouse gases, while aerosols and ozone use either ScenarioMIP emissions or CMIP-provided concentrations; output is distributed through the Earth System Grid Federation (ESGF).
- Figures use the simple climate model MAGICC version 6.8.01 BETA to calculate concentration, forcing, and temperature outcomes; no new climate model simulations are analyzed in this paper.
Limitations
- The paper states that IAM feasibility is not the same as real-world feasibility; not all scenarios may be equally attainable, and under limited technology availability or delayed mitigation some models find the 2.6 W m⁻² target unattainable.
- The paper states an open question is whether different SSPs reaching the same global forcing produce different climate outcomes; if sensitivity is larger than assumed, ESM simulations specific to each SSP–forcing combination would be required. It also notes concentration-driven scenarios cannot assess amplification effects of biogeochemical feedbacks beyond the provided GHG concentrations.
- Evident from the text: this is a design paper without a comprehensive analysis plan or results; it also notes pattern scaling and other emulators are not yet demonstrated to reliably replace climate model projections.
Model-written summary. Check it against the paper before relying on it.
Integrity signals
Registry
Cites
Statistics
Claims the paper makes
12 of 29 cited sources checked · 7 supported · 0 flagged · accuracy not yet measured
- Premisecitation
More recent work has refined this view, indicating that regional temperature outcomes that are statistically significantly different at a 5 % level for more than half the land surface area, and robustly so across the multi-model ensemble, require a separation of at least 0.3°C in global average temperature.
“More recent work (Tebaldi et al., 2015) has refined this view, indicating that regional temperature outcomes that are statistically significantly different at a 5 % level for more than half the land surface area, and robustly so across the multi-model ensemble, require a separation of at least 0.3 • C in global average temperature.”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Tebaldi et al., 2015 source
- Premisecitation
Not all scenarios considered in ScenarioMIP may be equally attainable.
“Results from major international IAM comparison projects (Clarke et al., 2009;Kriegler et al., 2014b;Riahi et al., 2015) indicate that not all scenarios considered in ScenarioMIP may be equally attainable.”
Quote in the paperNot a substantial claim2 of 3 sources checked- cites Clarke et al., 2009 source
Sections 3 and 8 (page numbers not provided) show that the EMF 22 climate-action cases differed in difficulty: no team produced all ten, and some targets could not be met by any model under delayed participation. That supports the general point that scenarios may differ in attainability, but this paper examines EMF 22 cases, not the scenarios considered in ScenarioMIP. (LLM, conf=0.84)
Experimental — accuracy not yet measured - cites Kriegler et al., 2014b
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- cites Riahi et al., 2015 source
Section 5, “Mitigation costs and feasibility,” reports that some modeled pathways were infeasible and that feasibility varied with near-term emissions and technology assumptions. This supports the general point that scenarios may differ in attainability, but the paper studies AMPERE pathways, not the scenarios considered in ScenarioMIP. (LLM, conf=0.84)
Experimental — accuracy not yet measured
- Premisecitation
The feasibility of a scenario in the real world hinges on additional factors, such as political and social concerns, which might render feasible model solutions unattainable.
“The latter hinges on a number of additional factors, such as political and social concerns, which might render feasible model solutions unattainable in the real world (see, e.g, Riahi et al., 2015).”
Quote in the paperNot a substantial claim1 of 1 sources checked- cites Riahi et al., 2015 source
- Premisecitation
For regional precipitation, a much wider separation is required to ensure that scenarios are statistically different.
“For regional precipitation, a much wider separation is required to ensure that scenarios are statistically different.”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Tebaldi et al., 2015 source
The Sensitivity of regional climate section finds that precipitation changes require a much larger difference in global average temperature than regional temperature changes to become statistically significant over much of the land surface. But the Discussion and conclusions says the authors cannot establish an absolute criterion for scenario separation; the results do not show that any particular separation will ensure statistically different precipitation outcomes. (LLM, conf=0.83)
Experimental — accuracy not yet measured
- Findingreasoning
SSP3-7.0 combines relatively high societal vulnerability (SSP3) with relatively high forcing.
“In addition, SSP3 (combined with this forcing pathway) is especially relevant to IAM/IAV studies because it combines relatively high societal vulnerability (SSP3) with relatively high forcing.”
Quote in the paperSubstantial claim
- Findingown data
SSP1-2.6 and its long-term extension are estimated to decline to 1.5 °C warming in the 22nd century.
“CMIP5 RCP2.6 projections, which have a median outcome across models of about 1.6 • C global mean surface temperature in 2100, and the SSP1-2.6 scenario and its long-term extension, which is estimated to decline to 1.5 • C warm- ing in the 22nd century (Fig. 5), can inform analyses of the implications of the 1.5 • C target.”
Quote in the paperNot a substantial claim - Findingreasoning
SSP2-4.5 combines intermediate societal vulnerability with an intermediate forcing level.
“and also because it is relevant to IAM/IAV research as a scenario that combines intermediate societal vulnerability with an intermediate forcing level.”
Quote in the paperSubstantial claim - Findingcitation
The SSP5-8.5 extension emissions pathway is estimated to produce equilibrated radiative forcing over the period 2200-2300 at a level similar to the long-term extension of RCP8.5, just above 12 W m-2 in the simple climate model used in Fig. 5.
“This emissions pathway is estimated to produce equilibrated radiative forcing over the period 2200-2300 at a level similar to the level reached in the long-term extension of RCP8.5 designed for CMIP5 (Meinshausen et al., 2011c; just above 12 W m -2 in the simple climate model used in Fig. 5).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Meinshausen et al., 2011c
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Findingown data
The SSP1-2.6 extension is expected to achieve a long-term equilibrium temperature of 1.25 °C above pre-industrial temperatures.
“This extension is expected to achieve a long-term equilibrium temperature of 1.25 • C above pre-industrial temperatures, based on the simple climate model used in Fig. 5.”
Quote in the paperNot a substantial claim - Findingreasoning
The SSP1-2.6 extension leads to slowly declining forcing that approximately stabilizes beyond 2200 around 2.0 W m-2.
“For SSP1-2.6 the rate of negative carbon emissions from fossil fuels reached in 2100 is extended to 2140 and then increases linearly to zero in 2185, with all other emissions (including CO 2 from land use) held constant at 2100 levels, leading to slowly declining forcing that approximately stabilizes beyond 2200 around 2.0 W m -2 .”
Quote in the paperNot a substantial claim - Findingnone given
SSP1 has substantial land use change, in particular increased global forest cover.
“SSP1 was chosen because it has substantial land use change (in particular increased global forest cover) and will be used by LUMIP to help address their scientific questions.”
Quote in the paperSubstantial claim - Findingnone given
SSP2's land use and aerosol pathways are not extreme relative to other SSPs.
“SSP2 was chosen because its land use and aerosol pathways are not extreme relative to other SSPs (and therefore appear as central for the concerns of DAMIP and DCPP)”
Quote in the paperSubstantial claim - Findingnone given
SSP5 is the only SSP scenario with emissions high enough to produce a radiative forcing of 8.5 W m-2 in 2100.
“SSP5 was chosen for this forcing pathway because it is the only SSP scenario with emissions high enough to produce a radiative forcing of 8.5 W m -2 in 2100.”
Quote in the paperSubstantial claim - Interpretationreasoning
The first objective of ScenarioMIP is considered to be the highest priority.
“The first objective is considered to be the highest priority for several reasons.”
Quote in the paperSubstantial claim - Premisecitation
Having common climate and socioeconomic scenarios serves as a critical means to enhance direct comparability of a wide variety of studies, allowing synthetic conclusions to be drawn that would not be possible from a variety of uncoordinated studies.
“Having common climate and socioeconomic scenarios serves as a critical means to enhance direct comparability of a wide variety of studies, allowing synthetic conclusions to be drawn that would not be possible from a variety of uncoordinated studies (van Vuuren et al., 2012;Kriegler et al., 2012).”
Quote in the paperSubstantial claim0 of 2 sources checked- cites van Vuuren et al., 2012
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- cites Kriegler et al., 2012 source
- Interpretationnone given
It was decided that identifying a smaller subset of scenarios by statistically sampling from combinations could currently not be carried out with a reasonable number of climate model simulations without sacrificing the representation of uncertainty for a given scenario.
“It was decided that this approach could currently not be carried out with a reasonable number of climate model simulations without sacrificing the representation of uncertainty for a given scenario.”
Quote in the paperSubstantial claim - Interpretationreasoning
A common set of scenarios for integration reduces the need for individual research projects to develop their own scenario information to support scenario-based studies.
“Finally, a common set of scenarios for integration reduces the need for individual research projects to develop their own scenario information to support scenario-based studies.”
Quote in the paperSubstantial claim - Study design and conductreasoning
The ScenarioMIP experimental design was developed collaboratively by researchers within the climate science, IAM, and IAV communities.
“Because of the importance of the ScenarioMIP simulations across multiple research fields and to policy makers, the experimental design was developed collaboratively by researchers within the climate science, IAM, and impacts, adaptation, and vulnerability (IAV) communities.”
Quote in the paperNot a substantial claim - Interpretationreasoning
The relatively high forcing level reached by SSP3-7.0 by the end of the 21st century will enable the exploration of potential changes in internal variability over a substantial range of global average radiative forcing and temperature change.
“The relatively high forcing level reached by this scenario by the end of the 21st century will enable the exploration of potential changes in internal variability over a substantial range of global average radiative forcing and temperature change, which could not be assessed if the large ensemble was run for a lower scenario, e.g.SSP2-4.5.”
Quote in the paperSubstantial claim- The authors state this as an assumption: Variability estimated for one scenario can be applied to outcomes for others.
- Premisecitation
The separation of model vs. scenario uncertainty is unclear in such an approach.
“We recognize that such an approach could be problematic for uncertainty analysis, as the separation of model vs. scenario uncertainty is unclear (Knutti and Sedláček, 2013).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Knutti and Sedláček, 2013 source
- Interpretationreasoning
The choice between concentration-and emissions-driven runs relates to a trade-off between the use of scenarios as means of integration across the different communities and the representation of model differences and overall uncertainty.
“The choice between concentration-and emissions-driven runs relates to a trade-off between the use of scenarios as means of integration across the different communities and the representation of model differences and overall uncertainty.”
Quote in the paperSubstantial claim - Interpretationreasoning
Concentration-driven scenarios do not allow for assessing amplification effects of biogeochemical feedbacks beyond what is included in the model used to generate the ScenarioMIP-provided GHG concentrations.
“In particular, concentration-driven scenarios do not allow for assessing amplification effects of biogeochemical feedbacks (e.g., in which climate change influences the carbon cycle, producing more emissions and more climate change, and further influencing the carbon cycle) beyond what is included in the model used to generate the ScenarioMIP-provided GHG concentrations.”
Quote in the paperSubstantial claim - Interpretationreasoning
The configuration used for the scenario simulations can benefit from the model evaluation over the historical period.
“In addition, this means that the configuration used for the scenario simulations can benefit from the model evaluation over the historical period.”
Quote in the paperNot a substantial claim - Premisenone given
CMIP5 RCP2.6 projections have a median outcome across models of about 1.6 °C global mean surface temperature in 2100.
“CMIP5 RCP2.6 projections, which have a median outcome across models of about 1.6 • C global mean surface temperature in 2100, and the SSP1-2.6 scenario and its long-term extension, which is estimated to decline to 1.5 • C warm- ing in the 22nd century (Fig. 5), can inform analyses of the implications of the 1.5 • C target.”
Quote in the paperNot a substantial claim - Premisecitation
Hall and Qu (2006) found that large inter-model variations in the seasonal cycle of the albedo between April and May in the 20th century are well correlated with similarly large inter-model variations in the snow-albedo feedback on climatological timescales.
“For example, Hall and Qu (2006) found that large inter-model variations in the seasonal cycle of the albedo between April and May in the 20th century are well correlated with similarly large inter-model variations in the snow-albedo feedback on climatological timescales.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Hall and Qu, 2006 source
- Interpretationnone given
The experimental design includes six out of eight 21st century scenarios that are within a maximum of 1.0 W m -2 of another scenario in terms of global average radiative forcing in 2100.
“The experimental design includes six out of eight 21st century scenarios that are within a maximum of 1.0 W m -2 of another scenario in terms of global average radiative forcing in 2100.”
Quote in the paperSubstantial claim - Interpretationnone given
One of the scenarios within the ScenarioMIP design describes a much stronger overshoot pathway with radiative forcing that peaks and declines within the 21st century and declines further thereafter.
“One of the scenarios within the ScenarioMIP design describes a much stronger overshoot pathway with radiative forcing that peaks and declines within the 21st century and declines further thereafter, allowing for investigation of the effect of overshoot and declining forcing on the climate system and society.”
Quote in the paperSubstantial claim - Interpretationown data
SSP1-2.6 is anticipated to produce a multi-model mean of significantly less than 2 °C warming by 2100.
“It is anticipated that it will produce a multi-model mean of significantly less than 2 • C warming by 2100 (Fig. 3), and therefore can support analyses of this policy goal.”
Quote in the paperSubstantial claim - Premisereasoning
In principle this forcing level can be achieved via pathways of emissions and land use that differ widely in terms of regional land use patterns, regional patterns of emissions of NTCFs, and mixes of global emissions of greenhouse gases (GHGs) and NTCFs.
“However, in principle this forcing level can be achieved via pathways of emissions and land use that differ widely in terms of regional land use patterns, regional patterns of emissions of NTCFs, and mixes of global emissions of greenhouse gases (GHGs) and NTCFs.”
Quote in the paperSubstantial claim - Interpretationnone given
ScenarioMIP is playing a key role by identifying an updated and expanded set of concentration pathways based on the SSPs to be run by climate models as part of CMIP6.
“ScenarioMIP is playing a key role by identifying an updated and expanded set of concentration pathways based on the SSPs to be run by climate models as part of CMIP6.”
Quote in the paperSubstantial claim - Premisecitation
Scenarios feasible to produce in an IAM that are significantly below RCP2.6 in terms of radiative forcing are currently rare and have only recently become available in the peer reviewed literature.
“Scenarios feasible to produce in an IAM that are significantly below RCP2.6 in terms of radiative forcing are currently rare and have only recently become available in the peer reviewed literature (Rogelj et al., 2015).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Rogelj et al., 2015 source
- Interpretationreasoning
Scenarios in the ScenarioMIP design are selected from these marker scenarios.
“Scenarios in the ScenarioMIP design are selected from these marker scenarios.”
Quote in the paperSubstantial claim - Premisecitation
Under specific conditions such as limited availability of technologies or delayed mitigation, some models find the low forcing target of 2.6 W m-2 unattainable.
“For example, under specific conditions (e.g., limited availability of technologies or delayed mitigation) some models find the low forcing target of 2.6 W m -2 unattainable.”
Quote in the paperNot a substantial claim - Premisenone given
The rows of the SSP forcing matrix shown in Fig. 1 are defined by forcing pathways that achieve the same level of global average radiative forcing in 2100.
“The rows of the SSP forcing matrix shown in Fig. 1 are defined by forcing pathways that achieve the same level of global average radiative forcing in 2100.”
Quote in the paperSubstantial claim - Premisecitation
Early in the design of the scenario framework, a criterion for selecting RCPs was that they be well separated in terms of radiative forcing.
“Early in the design of the scenario framework, a criterion for selecting RCPs was that they be well separated in terms of radiative forcing (Moss et al., 2008).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Moss et al., 2008
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Premisecitation
Current IAM runs have shown that combinations of socioeconomic development pathway and forcing pathway in the SSP-RCP scenario matrix are feasible.
“Each cell in the matrix indicates a combination of socioeconomic development pathway (i.e., an SSP) and climate outcome based on a particular forcing pathway that current IAM runs have shown to be feasible(Riahi et al., 2016).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Riahi et al., 2016
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Premisenone given
For CMIP6, natural forcings (solar and volcanic) will differ from those used in CMIP5.
“For CMIP6, these forcings will differ from what was used in CMIP5.”
Quote in the paperNot a substantial claim
- Classified as probably not a substantial claim. 29
- May combine two claims. 25
Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
PremisecitationThe RCPs were the basis for climate model projections in CMIP5 and their assessment in the IPCC AR5.
“The RCPs were the basis for climate model projections in CMIP5 (Taylor et al., 2012) and their assessment in the IPCC AR5 (IPCC, 2013).”
Quote in the paperNot a substantial claim1 of 2 sources checked- cites Taylor et al., 2012 source
- cites IPCC, 2013
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
PremisecitationSSPs 1 and 5 envision relatively optimistic trends for human development, with substantial investments in education and health, rapid economic growth, and well-functioning institutions.
“SSPs 1 and 5 envision relatively optimistic trends for human development, with substantial investments in education and health, rapid economic growth, and well-functioning institutions.”
Quote in the paperNot a substantial claim1 of 1 sources checked- cites O'Neill et al., 2015 source
May combine two claims.
PremisecitationInitial studies indicate that scenario differences of at least 0.3°C in global average surface temperature are likely necessary to generate statistically significant differences in local temperature over a substantial fraction of the surface, and substantially larger differences are required to produce similarly significant and extensive differences in precipitation outcomes.
“Initial studies indicate that scenario differences of at least 0.3 • C in global average surface temperature are likely necessary to generate statistically significant differences in local temperature over a substantial fraction of the surface, and substantially larger differences are required to produce similarly significant and extensive differences in precipitation outcomes (Tebaldi et al., 201”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Tebaldi et al., 2015 source
May combine two claims.
PremisecitationUnlike in CMIP3 and CMIP5, where climate model projections were part of the core experiments, in CMIP6 they are part of a dedicated CMIP6-Endorsed MIP.
“Unlike in CMIP3 and CMIP5, where climate model projections were part of the core experiments, in CMIP6 they are part of a dedicated CMIP6-Endorsed MIP (Eyring et al., 2016).”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Eyring et al., 2016 source
The Impacts section says future scenario experiments were part of the CMIP5 core experiments and will instead be run through ScenarioMIP in CMIP6. The passage does not establish the claim that projections were also core experiments in CMIP3. (LLM, conf=0.87)
Experimental — accuracy not yet measured
Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
PremisecitationSSP5 assumes an energy intensive, fossil-based economy, while in SSP1 there is an increasing shift toward sustainable practices.
“However, SSP5 assumes an energy intensive, fossilbased economy, while in SSP1 there is an increasing shift toward sustainable practices.”
Quote in the paperNot a substantial claim1 of 1 sources checked- cites O'Neill et al., 2015 source
Probably not a substantial claim: may not pass S3 (load-bearing).
PremisecitationSSP2 envisions a central pathway in which trends continue their historical patterns without substantial deviations.
“SSP2 envisions a central pathway in which trends continue their historical patterns without substantial deviations.”
Quote in the paperNot a substantial claim1 of 1 sources checked- cites O'Neill et al., 2015 source
Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
PremisecitationSSPs 3 and 4 envision more pessimistic development trends, with little investment in education or health, fast growing population, and increasing inequalities.
“SSPs 3 and 4 envision more pessimistic development trends, with little investment in education or health, fast growing population, and increasing inequalities.”
Quote in the paperNot a substantial claim1 of 1 sources checked- cites O'Neill et al., 2015 source
Section 4 says SSPs 3 and 4 have high population growth, slow economic growth and compounded inequality. Sections 3.3–3.4 describe declining or unequal investment in education and difficulty providing health care to disadvantaged groups. They do not establish uniformly little investment in health, or little education investment across all groups in SSP4. (LLM, conf=0.85)
Experimental — accuracy not yet measured
May combine two claims.
FindingreasoningMultiple IAM groups producing SSP-based scenarios have been able to produce preliminary scenarios based on SSP1 that reach about 1.9 W m-2 in 2100, leading to a likely (>66%) probability of staying below 1.5 °C in 2100, but a lower probability around mid-century.
“Multiple IAM groups producing SSP-based scenarios have been able to produce preliminary scenarios based on SSP1 that reach about 1.9 W m -2 in 2100, leading to a likely (> 66 %) probability of staying below 1.5 • C in 2100 (but a lower probability around mid-century).”
Quote in the paperSubstantial claimMay combine two claims.
Findingnone givenThe SSP5-3.4-OS extension produces a global mean temperature that equilibrates at about 1.25 °C above pre-industrial temperatures beyond 2200, but with a higher peak temperature of about 2.4 °C during the 21st century.
“Like the SSP1-2.6 extension, this pathway also produces a global mean temperature that equilibrates at about 1.25 • C above pre-industrial temperatures beyond 2200, but with a higher peak temperature (about 2.4 • C) during the 21st century.”
Quote in the paperNot a substantial claim- The authors state this as an assumption: The level of negative CO2 emissions from fossil fuels reached in 2100 remains constant until 2140, and then increases linearly to reach zero by 2190.
May combine two claims.
Findingnone givenSSP3-7.0 has relatively strong land use change and high emissions of NTCFs, unlike SSP5-8.5.
“SSP3-7.0 has relatively strong land use change and high emissions of NTCFs (unlike the SSP5-8.5 scenario), and therefore has been identified as an important experiment on which variants will be conducted by LU-MIP and AerChemMIP”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Findingnone givenSSP1-2.6 combines low vulnerability with low challenges for mitigation as well as a low forcing signal.
“From the IAM/IAV perspective this scenario is highly relevant since it combines low vulnerability with low challenges for mitigation as well as a low forcing signal.”
Quote in the paperNot a substantial claimMay combine two claims.
Findingnone givenSSP3-7.0 has both substantial land use change, in particular decreased global forest cover, and high NTCF emissions, particularly SO2.
“SSP3 was chosen because SSP3-7.0 is a scenario with both substantial land use change (in particular decreased global forest cover) and high NTCF emissions (particularly SO 2 ) and therefore will play an important role in LUMIP and AerChemMIP”
Quote in the paperSubstantial claimClassified as probably not a substantial claim. May combine two claims.
Findingnone givenThe two LUMIP scenarios, SSP3-7.0 and SSP1-2.6, differ both in forcing levels, spanning a range of approximately 4.5 W m-2 by 2100, and in land use change, with substantial deforestation in SSP3-7.0 and net afforestation in SSP1-2.6.
“The two scenarios would differ both in forcing levels, spanning a range of approximately 4.5 W m -2 by 2100, and in land use change, with substantial deforestation in the SSP3-7.0scenario and net afforestation in SSP1-2.6.”
Quote in the paperSubstantial claimClassified as probably not a substantial claim.
Interpretationnone givenScenarioMIP is the primary activity within CMIP6 that will provide multi-model climate projections based on alternative scenarios of future emissions and land use changes produced with integrated assessment models.
“The Scenario Model Intercomparison Project (Scenar-ioMIP) is the primary activity within Phase 6 of the Coupled Model Intercomparison Project (CMIP6) that will provide multi-model climate projections based on alternative scenarios of future emissions and land use changes produced with integrated assessment models.”
Quote in the paperSubstantial claimMay combine two claims.
InterpretationreasoningCMIP6 climate projections will differ from those in CMIP5 not only because they are produced with updated versions of climate models, but also because they are driven with SSP-based scenarios produced with updated versions of IAMs and based on updated data on recent emissions trends.
“CMIP6 climate projections will differ from those in CMIP5 not only because they are produced with updated versions of climate models, but also because they are driven with SSP-based scenarios produced with updated versions of IAMs and based on updated data on recent emissions trends.”
Quote in the paperSubstantial claimMay combine two claims.
Interpretationnone givenThe ScenarioMIP design consists of eight alternative 21st century scenarios plus one large initial condition ensemble and a set of long-term extensions, divided into two tiers defined by relative priority.
“a design has been identified consisting of eight alternative 21st century scenarios plus one large initial condition ensemble and a set of long-term extensions, divided into two tiers defined by relative priority.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Premisenone givenThe SSPs describe alternative evolutions of future society in the absence of climate change or climate policy.
“In short, the SSPs describe alternative evolutions of future society in the absence of climate change or climate policy.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim.
PremisecitationA workshop concluded that pattern scaling has currently not yet been demonstrated to be able to reliably replace the need for climate model projections to generate information for impact studies.
“A workshop held for this purpose concluded that pattern scaling has currently not yet been demonstrated to be able to reli-ably replace the need for climate model projections to generate information for impact studies”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Tebaldi and Arblaster, 2014 source
May combine two claims.
PremisecitationIAM scenarios were developed based on the SSPs by elaborating on their implications for energy systems and land use changes and quantifying resulting greenhouse gas emissions and atmospheric concentrations.
“IAM scenarios were then developed based on the SSPs by elaborating on their implications for energy systems (Bauer et al., 2016) and land use changes (Popp et al., 2016) and quantifying resulting greenhouse gas emissions and atmospheric concentrations (Riahi et al., 2016).”
Quote in the paperSubstantial claim0 of 3 sources checked- cites Bauer et al., 2016
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- cites Popp et al., 2016
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- cites Riahi et al., 2016
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
Classified as probably not a substantial claim.
InterpretationreasoningThese CMIP6 simulations will allow integrated analyses to be carried out using climate simulations based on the latest versions of climate models, for a larger set of concentration pathways based on the most recent versions of IAMs.
“These CMIP6 simulations will allow integrated analyses to be carried out using climate simulations based on the latest versions of climate models, for a larger set of concentration pathways based on the most recent versions of IAMs.”
Quote in the paperSubstantial claim- The authors state this as an assumption: Differences in climate outcomes between land use and emissions pathways that achieve the same global average radiative forcing level in 2100 but have different patterns of regional forcing are likely to be small relative to the overall uncertainty in applications of these simulations to integrated analyses (including impact assessments).
Probably not a substantial claim: may not pass S3 (load-bearing).
Interpretationnone givenThere might be feasible developments in the real world that are not anticipated by the IAM.
“There might also be feasible developments in the real world that are not anticipated by the IAM.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
PremisecitationThese SSP-based IAM scenarios consist of a set of baseline scenarios, which provide a description of future developments in the absence of climate change impacts or new climate policies beyond those in place today, as well as mitigation scenarios which explore the implications of climate change mitigation policies applied to the baseline scenarios.
“These SSP-based IAM scenarios consist of a set of baseline scenarios, which provide a description of future developments in the absence of climate change impacts or new climate policies beyond those in place today, as well as mitigation scenarios which explore the implications of climate change mitigation policies applied to the baseline scenarios.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Riahi et al., 2016
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
PremisecitationClimate model emulators have the potential to provide a computationally efficient means of generating climate outcomes for arbitrary scenarios and, in so doing, facilitate the representation of uncertainty in applications to impact studies.
“Climate model emulators have the potential to provide a computationally efficient means of generating climate outcomes for arbitrary scenarios and, in so doing, facilitate the representation of uncertainty in applications to impact studies (Tebaldi and Arblaster, 2014).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Tebaldi and Arblaster, 2014 source
Classified as probably not a substantial claim.
Interpretationnone givenScenarioMIP simulations will be key to addressing two of the three CMIP6 science questions that have informed the overall CMIP6 design and the endorsement of proposed MIPs, related to the effects of external forcings on the Earth system and to the confounding effects of different sources of uncertainty on future anthropogenic climate change outcomes.
“However in addition, ScenarioMIP simulations will be key to addressing two of the three CMIP6 science questions that have informed the overall CMIP6 design and the endorsement of proposed MIPs, related to the effects of external forcings on the Earth system and to the confounding effects of different sources of uncertainty on future anthropogenic climate change outcomes.”
Quote in the paperSubstantial claimMay combine two claims.
PremisecitationMultiple IAMs were used for the quantification of the SSP scenarios, and a single marker scenario was selected as representative in each case.
“Multiple IAMs were used for the quantification of the SSP scenarios, and a single”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Riahi et al., 2016
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
Classified as probably not a substantial claim.
InterpretationreasoningFeasibility in an IAM model needs to be strictly differentiated from the feasibility of a scenario in the real world.
“Feasibility in an IAM model needs to be strictly differentiated, however, from the feasibility of a scenario in the real world, i.e. whether or not the scenario is capable of being attained.”
Quote in the paperSubstantial claimMay combine two claims.
InterpretationreasoningThis difference in global temperature is roughly equivalent to about 0.75 W m -2 of global average forcing in an idealized 1 % yr -1 CO 2 increase experiment, although the equivalent value is sensitive to the forcing pathway.
“This difference in global temperature is roughly equivalent to about 0.75 W m -2 of global average forcing in an idealized 1 % yr -1 CO 2 increase experiment, although the equivalent value is sensitive to the forcing pathway.”
Quote in the paperSubstantial claimMay combine two claims.
Interpretationnone givenThe ScenarioMIP experimental design consists of a set of eight pathways of future emissions, concentrations and land use, with additional ensemble members and long-term extensions, grouped into two tiers of priority (of which only the first constitutes a required set for modeling centers participating in ScenarioMIP).
“The ScenarioMIP experimental design consists of a set of eight pathways of future emissions, concentrations and land use, with additional ensemble members and long-term extensions, grouped into two tiers of priority (of which only the first constitutes a required set for modeling centers participating in ScenarioMIP).”
Quote in the paperSubstantial claimClassified as probably not a substantial claim.
Interpretationnone givenThe ScenarioMIP design will include an updated and expanded set of forcing pathways directly derived from SSPs.
“The ScenarioMIP design will include an updated and expanded set of forcing pathways directly derived from SSPs.”
Quote in the paperSubstantial claimClassified as probably not a substantial claim.
Study design and conductreasoningThe scenario simulations specified in ScenarioMIP are to be performed in the same configuration as the one used in the CMIP6 historical simulations, ensuring continuity in the climate simulations.
“The scenario simulations specified in ScenarioMIP are to be performed in the same configuration as the one used in the CMIP6 historical simulations, ensuring continuity in the climate simulations.”
Quote in the paperSubstantial claimMay combine two claims.
InterpretationreasoningThe SSP5-3.4-OS extension can be seen as an overshoot of the 3.4 W m-2 level and of the 2.6 W m-2 level.
“In this way, the scenario can be seen as an overshoot of the 3.4 W m -2 level (which it exceeds and then returns to by about 2100) and of the 2.6 W m -2 level, which it returns to in the first half of the 22nd century.”
Quote in the paperNot a substantial claimMay combine two claims.
Premisenone givenCMIP6 climate projections will differ from those for CMIP5 due to a new generation of climate models, a new start year for the future scenarios (2015 for CMIP6 vs. 2006 for CMIP5), as well as a new set of scenarios of concentrations, emissions, and land use.
“CMIP6 climate projections will differ from those for CMIP5 due to a new generation of climate models, a new start year for the future scenarios (2015 for CMIP6 vs. 2006 for CMIP5), as well as a new set of scenarios of concentrations, emissions, and land use (Figs. 3 and 4).”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S4 (based). May combine two claims.
Interpretationnone givenThe state of development of such emulators is such that many situations remain where they are not suitable, their behavior deviating significantly from the more computationally complex, physically based models that they seek to emulate, or falling short of producing temporally coherent projections, or projections of multiple variables physically inter-related.
“However, the state of development of such emulators is such that many situations remain where they are not suitable, their behavior deviating significantly from the more computationally complex, physically based models that they seek to emulate, or falling short of producing temporally coherent projections, or projections of multiple variables physically inter-related.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing), S4 (based).
Premisenone givenThe lowest RCP (RCP2.6), and the low SSP scenarios, already exhibit a limited degree of concentration overshoot.
“The lowest RCP (RCP2.6), and the low SSP scenarios, already exhibit a limited degree of concentration overshoot.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Interpretationnone givenScenarioMIP will carry out climate model simulations for one particular land use and concentration pathway that leads to this level of radiative forcing.
“ScenarioMIP will carry out climate model simulations for one particular land use and concentration pathway that leads to this level of radiative forcing.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S4 (based).
Interpretationnone givenThe multi-model approach will allow for a better characterization of uncertainty in climate outcomes than would otherwise be possible.
“The multi-model approach will allow for a better characterization of uncertainty in climate outcomes than would otherwise be possible”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Premisenone givenResearchers examining the consequences of climate change and potential adaptations are a key user group of CMIP outputs and products.
“Researchers examining the consequences of climate change and potential adaptations are a key user group of CMIP outputs and products.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S2 (checkable), S4 (based).
Interpretationnone givenIntegrating climate simulations from ScenarioMIP with the SSPs or other characterizations of societal futures will allow for analyses of future mitigation, adaptation, and impacts that account for both climate and societal change in a coherent fashion.
“Integrating climate simulations from ScenarioMIP with the SSPs or other characterizations of societal futures will allow for analyses of future mitigation, adaptation, and impacts that account for both climate and societal change in a coherent fashion.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim. May combine two claims.
Interpretationnone givenThe ScenarioMIP design calls for a large initial condition ensemble that will allow for representation of internal variability in impact studies and improved signal detection in experiments in other MIPs that carry out variants of this scenario.
“and the design also calls for a large initial condition ensemble that will allow for representation of internal variability in impact studies as well as improved signal detection in experiments in other MIPs that will carry out variants of this scenario.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Premisenone givenFuture climate model simulations require specification of natural forcings, in particular solar forcing and volcanic emissions.
“Future simulations will also require specification of natural forcings, in particular solar forcing and volcanic emissions.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim.
InterpretationreasoningThe climate model output from the scenarios allows for sector-specific indices being derived.
“In particular ScenarioMIP will link with the VIACS Advisory Board to ensure that the climate model output from the scenarios allows for sector-specific indices being derived (e.g., heat damage degree days for ecosystems, consecutive dry days for agriculture and water resources).”
Quote in the paperSubstantial claimClassified as probably not a substantial claim.
Premisenone givenData sets for future natural and anthropogenic forcings are required in order to run the ScenarioMIP experiments.
“In order to run the experiments, data sets for future natural and anthropogenic forcings are required.”
Quote in the paperSubstantial claimClassified as probably not a substantial claim. May combine two claims.
Interpretationnone givenMulti-model climate model projections from ScenarioMIP will provide the basis for investigating targeted scientific questions regarding the role of specific forcings, the contribution of forcing uncertainty to the total uncertainty budget, the effect of a peak and decline in forcing, and long-term climate system outcomes beyond the 21st century.
“Multi-model climate model projections from ScenarioMIP will also provide the basis for investigating a number of targeted scientific questions regarding the role of specific forcings and the contribution of forcing uncertainty to the total uncertainty budget, the effect of a peak and decline in forcing, and longterm climate system outcomes beyond the 21st century.”
Quote in the paperSubstantial claim
The authors state this as an assumption.
Differences in climate change projections between RCP-based and SSPx-y simulations following a similar global forcing pathway would be small enough to still warrant integration of the two sets of information into mitigation, impacts and adaptation analysis.
“An enabling hypothesis of the parallel process is that differences in climate change projections would be small enough to still warrant integration of the two sets of information into mitigation, impacts and adaptation analysis.”
The authors state this as an assumption.
Differences in climate outcomes between land use and emissions pathways that achieve the same global average radiative forcing level in 2100 but have different patterns of regional forcing are likely to be small relative to the overall uncertainty in applications of these simulations to integrated analyses (including impact assessments).
“An assumption underlying the parallel process (Moss et al., 2010) and the SSP scenario framework is that these differences in climate outcomes are likely to be small relative to the overall uncertainty in applications of these simulations to integrated analyses (including impact assessments).”
The authors state this as an assumption.
Variability estimated for one scenario can be applied to outcomes for others.
“based on the assumption that variability estimated for one scenario can be applied to outcomes for others.”
The authors state this as an assumption.
The level of negative CO2 emissions from fossil fuels reached in 2100 remains constant until 2140, and then increases linearly to reach zero by 2190.
“The extension assumes that the level of negative CO 2 emissions from fossil fuels reached in 2100 remains constant until 2140, and then increase linearly to reach zero by 2190.”
The paper relies on this without support.
Differences in climate outcomes produced by different scenarios for the same global forcing pathway are likely small relative to regional climate variability, uncertainty across climate models, and uncertainty in impact models used to investigate outcomes of interest to the IAV community.
“The prevailing hypothesis is that differences in climate outcomes produced by different scenarios for the same global forcing pathway are likely small relative to regional climate variability, uncertainty across climate models, and uncertainty in impact models used to investigate outcomes of interest to the IAV community (see Sect. 2.4.2).”
The authors state this as an assumption.
The temperature projections in Figure 3 assume zero volcanic forcing and maintain 11-year solar forcing cycles, consistent with the CMIP5 approach.
“projections assume zero volcanic forcing and maintain 11-year solar forcing cycles, consistent with the CMIP5 approach(Meinshausen et al., 2011c).”
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Self-citationJONES, C. D., Arora, V. K., Friedlingstein, P., Bopp, L., Brovkin, V. A., Dunne, J. P. P., Graven, H., Hoffman, F. M., Ilyina, T., John, J. G., et al. (2016) · Geoscientific model development · doi:10.5194/gmd-9-2853-2016 · Cited by 397 · cited 2× · see citing works
“…study couplings be-tween land use changes and atmospheric chemistry Coupled Climate Carbon Cycle MIP (C MIP) ScenarioMIP will coordinate with C MIP (Jones et al., 2016) on targeted scenarios regarding concentration vs. emission-driven simulations While the ScenarioMIP protocol will request CO 2…”
Self-citationIce Sheet Model Intercomparison Project (ISMIP6) contribution to CMIP6
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“ISMIP6 (Nowicki et al., 2016) will be proposing two types of experiments that will draw on long-term extensions of a scenario from ScenarioMIP in order to investigate ice sheet response and ice–climate interactions on centennial timescales.”
Riahi, K., Kriegler, E., Johnson, N., Bertram, C., den Elzen, M., Eom, J., Schaeffer, M., Edmonds, J., Isaac, M., Krey, V., et al. (2015) · Technological Forecasting and Social Change · doi:10.1016/j.techfore.2013.09.016 · Cited by 360 · see citing works
Self-citationEnsemble flood risk assessment in Europe under high end climate scenarios
Alfieri, L., Feyen, L., Dottori, F., & Bianchi, A. (2015) · Global Environmental Change · doi:10.1016/j.gloenvcha.2015.09.004 · Cited by 329 · see citing works
The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6
Pincus, R. L., Forster, P. M. D. F., & Stevens, B. (2016) · Geoscientific model development · doi:10.5194/gmd-9-3447-2016 · Cited by 322 · see citing works
AerChemMIP: quantifying the effects of chemistry and aerosols in CMIP6
Collins, W., Lamarque, J., Schulz, M., Boucher, O., Eyring, V., Hegglin, M., Maycock, A., Myhre, G., Prather, M., Shindell, D., et al. (2016) · Geoscientific model development · doi:10.5194/gmd-10-585-2017 · Cited by 319 · cited 2× · see citing works
“AerChemMIP (Collins et al., 2016) has a Tier 1 experiment (with additional Tier 2 and 3 related studies) directed at the sensitivity of climate to near-term climate forcers.”
Self-citationvan Vuuren, D. P., Riahi, K., Moss, R. H., Edmonds, J., Thomson, A. M., Nakićenović, N., Kram, T., Berkhout, F., Swart, R. J., Janetos, A. C., et al. (2011) · Global Environmental Change · doi:10.1016/j.gloenvcha.2011.08.002 · Cited by 316 · see citing works
Self-citationSeptember sea-ice cover in the Arctic Ocean projected to vanish by 2100
Boé, J., Hall, A. D., & Qu, X. (2009) · Nature Geoscience · doi:10.1038/ngeo467 · Cited by 307 · cited 1× · see citing works
“, 2014), and relations of past and future sea ice or temperature trends (Boé et al., 2009; Knutti and Tomassini, 2008; Mahlstein and Knutti, 2012; Massonet et al., 2012).”
Kravitz, B., Robock, A., Tilmes, S., Boucher, O., English, J. M., Irvine, P. J., Jones, A., Lawrence, M. G., MacCracken, M., Muri, H., et al. (2015) · Geoscientific Model Development · doi:10.5194/gmd-8-3379-2015 · Cited by 297 · see citing works
Arnell, N. W., & Lloyd-Hughes, B. (2013) · Climatic Change · doi:10.1007/s10584-013-0948-4 · Cited by 283 · see citing works
Pattern scaling: Its strengths and limitations, and an update on the latest model simulations
Tebaldi, C., & Arblaster, J. M. (2014) · Climatic Change · doi:10.1007/s10584-013-1032-9 · Cited by 274 · cited 2× · see citing works
“Climate model emulators have the potential to provide a computationally efficient means of generating climate outcomes for arbitrary scenarios and, in so doing, facilitate the representation of uncertainty in applications to impact studies (Tebaldi and Arblaster, 2014).”
Self-citationConstraining projections of summer Arctic sea ice
Massonnet, F., Fichefet, T., Goosse, H., Bitz, C. M., Philippon, G., Holland, M. M., & Barriat, P.-Y. (2012) · The Cryosphere · doi:10.5194/tc-6-1383-2012 · Cited by 265 · see citing works
van Vuuren, D. P., Edmonds, J., Kainuma, M., Riahi, K., & Weyant, J. P. (2011) · Climatic Change · doi:10.1007/s10584-011-0157-y · Cited by 244 · cited 2× · see citing works
“This process will basically be done using the methods applied earlier for the RCPs (Van Vuuren et al., 2011a).”
Self-citationClimate Model Intercomparisons: Preparing for the Next Phase
Meehl, G. A., Moss, R. H., Taylor, K. E., Eyring, V., Stouffer, R. J., Bony, S., & Stevens, B. (2014) · Eos · doi:10.1002/2014eo090001 · Cited by 189 · see citing works
Self-citationEmergent Constraints for Cloud Feedbacks
Klein, S. A., & Hall, A. D. (2015) · Current Climate Change Reports · doi:10.1007/s40641-015-0027-1 · Cited by 188 · cited 1× · see citing works
“, 2016), cloud feedbacks and equilibrium climate sensitivity (Huber et al., 2011; Fasullo and Trenberth, 2012; Fasullo et al., 2015; Klein and Hall, 2015; Knutti et al., 2006; Sherwood et al., 2014), and relations of past and future sea ice or temperature trends (Boé et al.”
Constraining Climate Sensitivity from the Seasonal Cycle in Surface Temperature
Knutti, R., Meehl, G. A., Allen, M. R., & Stainforth, D. A. (2006) · Journal of Climate · doi:10.1175/jcli3865.1 · Cited by 183 · cited 1× · see citing works
“, 2016), cloud feedbacks and equilibrium climate sensitivity (Huber et al., 2011; Fasullo and Trenberth, 2012; Fasullo et al., 2015; Klein and Hall, 2015; Knutti et al., 2006; Sherwood et al., 2014), and relations of past and future sea ice or temperature trends (Boé et al.”
Self-citationMeinshausen, M. A., Wigley, T. M. L., & Raper, S. C. B. (2011) · Atmospheric chemistry and physics · doi:10.5194/acp-11-1457-2011 · Cited by 179 · cited 6× · see citing works
“The climate model output from ScenarioMIP experiments described in this paper will be distributed through the Earth System Grid Federation (ESGF) with DOIs assigned. in CMIP5, the model output will be freely accessible through data portals after registration.”
InfluentialA Less Cloudy Future: The Role of Subtropical Subsidence in Climate Sensitivity
Fasullo, J., & Trenberth, K. E. (2012) · Science · doi:10.1126/science.1227465 · Cited by 166 · see citing works
Hejazi, M. I., Voisin, N., Liu, L., Bramer, L. M., Fortin, D. C., Hathaway, J. E., Huang, M., Kyle, P., Leung, L. R., Li, H.-Y., et al. (2015) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1421675112 · Cited by 166 · cited 2× · see citing works
“…the CMIP5 simulations of the RCPs have already begun to appear (e.g., Alfieri et al., 2015; Arnell et al., 2014; Biewald et al., 2015; Dong et al., 2015; Hejazi et al., 2015) and climate model simulations with the RCPs will continue to be a key input to research on climate change and impacts for…”
Assessing Transformation Pathways
(2015) · Climate Change 2014: Mitigation of Climate Change · doi:10.1017/cbo9781107415416.012 · Cited by 159 · cited 5× · see citing works
“Two of these fill in gaps between RCPs, one represents a substantial forcing overshoot pathway, and one investigates a forcing pathway below the RCP2.”
InfluentialSelf-citationSeptember Arctic sea ice predicted to disappear near 2°C global warming above present
Mahlstein, I., & Knutti, R. (2012) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jd016709 · Cited by 151 · see citing works
Self-citationEmergent constraints on climate‐carbon cycle feedbacks in the CMIP5 Earth system models
Wenzel, S., Cox, P. M., Eyring, V., & Friedlingstein, P. (2014) · Journal of Geophysical Research Biogeosciences · doi:10.1002/2013jg002591 · Cited by 149 · see citing works
Self-citationImproved pattern scaling approaches for the use in climate impact studies
Herger, N., Sanderson, B. M., & Knutti, R. (2015) · Geophysical Research Letters · doi:10.1002/2015gl063569 · Cited by 114 · cited 1× · see citing works
“…deliberately explores a large range of forcings (both with respect to a lower and upper end, recently found to be important in training emulators by Herger et al., 2015), non-traditional pathways like substantial overshoots and long-term extensions and, together with collaborating MIPs, the…”
Self-citationBracegirdle, T. J., & Stephenson, D. B. (2012) · Journal of Climate · doi:10.1175/jcli-d-12-00537.1 · Cited by 97 · cited 1× · see citing works
“A method to relate observed aspects of the present-day mean climate or recent trends to the Earth system response in some quantity is the so-called Emergent Constraints method (Allen and Ingram, 2002; Bracegirdle and Stephenson, 2013; Hall and Qu, 2006).”
Dong, W., Liu, Z., Liao, H., Tang, Q., & Li, X. (2015) · Climatic Change · doi:10.1007/s10584-015-1372-8 · Cited by 84 · cited 2× · see citing works
“Integrated analyses drawing on the qualitative and quantitative elements of the SSPs and climate change information from the CMIP5 simulations of the RCPs have already begun to appear (e.g., Alfieri et al., 2015; Arnell et al., 2014; Biewald et al., 2015; Dong et al., 2015; Hejazi et al., 2015) and climate model simul…”
Constraints on the transient climate response from observed global temperature and ocean heat uptake
Knutti, R., & Tomassini, L. (2008) · Geophysical Research Letters · doi:10.1029/2007gl032904 · Cited by 57 · see citing works
Self-citationConstraints on Climate Sensitivity from Radiation Patterns in Climate Models
Huber, M., Mahlstein, I., Wild, M., Fasullo, J., & Knutti, R. (2010) · Journal of Climate · doi:10.1175/2010jcli3403.1 · Cited by 50 · cited 1× · see citing works
“, 2016), cloud feedbacks and equilibrium climate sensitivity (Huber et al., 2011; Fasullo and Trenberth, 2012; Fasullo et al., 2015; Klein and Hall, 2015; Knutti et al., 2006; Sherwood et al., 2014), and relations of past and future sea ice or temperature trends (Boé et al.”
Self-citationRuane, A., Teichmann, C., Arnell, N., Carter, T. R., Ebi, K., Frieler, K., Goodess, C., Hewitson, B., Horton, R., Kovats, R., et al. (2016) · Geoscientific model development · doi:10.5194/gmd-9-3493-2016 · Cited by 46 · see citing works
Self-citationWenzel, S., Eyring, V., Gerber, E. P., et al. (2015) · Journal of Climate · doi:10.1175/jcli-d-15-0412.1 · Cited by 43 · cited 1× · see citing works
“, 2014), the Austral jet stream position (Wenzel et al., 2016), cloud feedbacks and equilibrium climate sensitivity (Huber et al.”
Self-citationThe Radiative Forcing Model Intercomparison Project (RFMIP): Experimental Protocol for CMIP6Preprint
Pincus, R. L., Forster, P. M. D. F., & Stevens, B. (2016) · doi:10.5194/gmd-2016-88 · Cited by 36 · see citing works
Sensitivity of regional climate to global temperature and forcing
Tebaldi, C., O’Neill, B., & Lamarque, J.-F. (2015) · Environmental Research Letters · doi:10.1088/1748-9326/10/7/074001 · Cited by 21 · cited 3× · see citing works
“3 C in global average surface temperature are likely necessary to generate statistically significant differences in local temperature over a substantial fraction of the surface, and substantially larger differences are required to produce similarly significant and extensive differences in precipitation outcomes (Tebal…”
InfluentialSelf-citationAerChemMIP: Quantifying the effects of chemistry and aerosols in CMIP6Preprint
Collins, W. J., Lamarque, J., Schulz, M., et al. (2016) · doi:10.5194/gmd-2016-139 · Cited by 21 · see citing works
Self-citationThe Decadal Climate Prediction ProjectPreprint
Boer, G. J., Smith, D. M., Cassou, C., et al. (2016) · doi:10.5194/gmd-2016-78 · Cited by 20 · cited 1× · see citing works
“distributions of emissions and concentrations of greenhouse gases, ozone concentrations (or precursors, for emissions-driven experiments), and aerosols and land use, at a level of spatial detail suitable for the generation of climate models that will be used in CMIP6.”
Recent Progress in Constraining Climate Sensitivity With Model Ensembles
Fasullo, J., Sanderson, B. M., & Trenberth, K. E. (2015) · Current Climate Change Reports · doi:10.1007/s40641-015-0021-7 · Cited by 17 · cited 1× · see citing works
“, 2016), cloud feedbacks and equilibrium climate sensitivity (Huber et al., 2011; Fasullo and Trenberth, 2012; Fasullo et al., 2015; Klein and Hall, 2015; Knutti et al., 2006; Sherwood et al., 2014), and relations of past and future sea ice or temperature trends (Boé et al.”
Self-citationA New Scenario Framework for Climate Change Research: The Concept of Shared Socioeconomic Pathways
O’Neill, B. C., Kriegler, E., Riahi, K., Ebi, K. L., & Stéphane Hallegatte, A. (2014) · Springer eBooks · doi:10.1596/23213 · Cited by 13 · see citing works
Self-citationDetection and Attribution Model Intercomparison Project (DAMIP)
Gillett, N. P., Shiogama, H., Funke, B., et al. (2016) · doi:10.5194/gmd-2016-74 · Cited by 12
Ice Sheet Model Intercomparison Project (ISMIP6) contribution to CMIP6
Nowicki, S. M. J., Payne, T., Larour, E., et al. (2016) · doi:10.5194/gmd-2016-105 · Cited by 9
Historical greenhouse gas concentrations
Meinshausen, M., Vogel, E., Nauels, A., et al. (2016) · doi:10.5194/gmd-2016-169 · Cited by 6
The Vulnerability, Impacts, Adaptation, and Climate Services (VIACS) Advisory Board for CMIP6
Ruane, A., Teichmann, C., Arnell, N., Carter, T. R., Ebi, K., Frieler, K., Goodess, C., Hewitson, B., Horton, R., Kovats, R., et al. (2016) · doi:10.5194/gmd-2016-71 · Cited by 4
Self-citationDeveloping Climate Model Comparisons
O’Neill, B. C., Lamarque, J., & Lawrence, D. M. (2014) · Eos · doi:10.1002/2014eo490008 · Cited by 3 · see citing works
Self-citationSupplementary material to "Historical greenhouse gas concentrations"
Meinshausen, M. A., Vogel, E., Nauels, A., et al. (2016) · doi:10.5194/gmd-2016-169-supplement · Cited by 2 · see citing works
Kriegler, E., Edmonds, J., Hallegatte, S., et al. (2014) · doi:10.1596/23214
Self-citationA New Scenario Framework for Climate Change Research: Scenario Matrix Architecture
van Vuuren, D. P., Kriegler, E., O’Neill, B. C., Ebi, K. L., & Riahi, K. (2014) · doi:10.1596/23212
Self-citation
Flagged first, then by citations
Research works printed but not linked: 4
- IPCC: Climate Change 2001: Mitigation of Climate Change, Contribution of Working Group III to the Third Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Davidson, O. R. and Mertz, B., Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 2001.
- IPCC: Climate Change 2013: The Physical Science Basis, Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Stocker, T. F., Qin, D., Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P. M., Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 1535 pp., 2013.
- IPCC: Climate Change 2014: Impacts, Adaptation, and Vulnerability. Part A: Global and Sectoral Aspects. Contribution of Working Group II to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Field, C. B., Barros, V. R., Dokken, D. J., Mach, K. J., Mastrandrea, M. D., Bilir, T. E., Chatterjee, M., Ebi, K. L., Estrada, Y. O., Genova, R. C., Girma, B., Kissel, E. S., Levy, A. N., MacCracken, S., Mastrandrea, P. R., and White, L. L., Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 1132 pp., 2014a.
- IPCC: Climate Change 2014: Impacts, Adaptation, and Vulnerability. Part B: Regional Aspects. Contribution of Working Group II to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Barros, V. R., Field, C. B., Dokken, D. J., Mastrandrea, M. D., Mach, K. J., Bilir, T. E., Chatterjee, M., Ebi, K. L., Estrada, Y. O., Genova, R. C., Girma, B., Kissel, E. S., Levy, A. N., MacCracken, S., Mastrandrea, P. R., and White, L. L., Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, 688 pp., 2014b.
Cited by
Sorted by citations
Riahi, K., van Vuuren, D. P., Kriegler, E., Edmonds, J., O’Neill, B. C., Fujimori, S., Bauer, N., Calvin, K., Dellink, R., Fricko, O., et al. (2017) · Global Environmental Change · doi:10.1016/j.gloenvcha.2016.05.009 · Cited by 6,607 · see citing works
“The narratives of the SSPs (O ’ Neill et al., 2016a) were developed using large expert teams that together designed the storylines and ensured their internal consistency.”
InfluentialSelf-citationThe Community Earth System Model Version 2 (CESM2)
Danabasoglu, G., Lamarque, J., Bacmeister, J. T., Bailey, D. A., DuVivier, A. K., Edwards, J., Emmons, L. K., Fasullo, J., García, R. R., Gettelman, A., et al. (2020) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms001916 · Cited by 3,273 · see citing works
“In addition, CESM2 is participating in about 20 Model Intercomparison Projects (MIPs) within CMIP6, including the ScenarioMIP, which requests future‐projection simulations driven by alternative plausible futures of emissions and land use (O'Neill et al., 2016).”
BackgroundSelf-citationThe Global Methane Budget 2000–2017
Saunois, M., Stavert, A. R., Poulter, B., Bousquet, P., Canadell, J. G., Jackson, R. B., Raymond, P. A., Dlugokencky, E. J., Houweling, S., Patra, P. K., et al. (2020) · Earth System Science Data · doi:10.5194/essd-12-1561-2020 · Cited by 2,711 · see citing works
A comprehensive quantification of global nitrous oxide sources and sinks
Tian, H., Xu, R., Canadell, J. G., Thompson, R. L., Winiwarter, W., Suntharalingam, P., Davidson, E. A., Ciais, P., Jackson, R. B., Janssens-Maenhout, G., et al. (2020) · Nature · doi:10.1038/s41586-020-2780-0 · Cited by 1,959 · see citing works
Future global urban water scarcity and potential solutions
He, C., Liu, Z., Wu, J., Pan, X., Fang, Z., Li, J., & Bryan, B. A. (2021) · Nature Communications · doi:10.1038/s41467-021-25026-3 · Cited by 1,952 · see citing works
“5 represents a rapid development pathway and very high radiative forcing 38 .”
BackgroundMethodInfluentialThe shared socio-economic pathway (SSP) greenhouse gas concentrations and their extensions to 2500
Meinshausen, M., Nicholls, Z. R. J., Lewis, J., Gidden, M. J., Vogel, E., Freund, M., Beyerle, U., Gessner, C., Nauels, A., Bauer, N., et al. (2020) · Geoscientific Model Development · doi:10.5194/gmd-13-3571-2020 · Cited by 1,815 · see citing works
Presentation and Evaluation of the IPSL‐CM6A‐LR Climate Model
Boucher, O., Servonnat, J., Albright, A. L., Aumont, O., Balkanski, Y. J., Bastrikov, V., Bekki, S., Bonnet, R., Bony, S., Bopp, L., et al. (2020) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms002010 · Cited by 1,762 · see citing works
Mauritsen, T., Bader, J., Becker, T., Behrens, J., Bittner, M., Brokopf, R., Brovkin, V. A., Claussen, M. A., Crueger, T., Esch, M., et al. (2019) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2018ms001400 · Cited by 1,527 · see citing works
Scenarios towards limiting global mean temperature increase below 1.5 °C
Rogelj, J., Popp, A., Calvin, K. V., Luderer, G., Emmerling, J., Gernaat, D., Fujimori, S., Strefler, J., Hasegawa, T., Marangoni, G., et al. (2018) · Nature Climate Change · doi:10.1038/s41558-018-0091-3 · Cited by 1,341 · see citing works
Self-citationUKESM1: Description and Evaluation of the U.K. Earth System Model
Sellar, A., Jones, C., Mulcahy, J. P., Tang, Y., Yool, A., Wiltshire, A., O’Connor, F. M., Stringer, M. A., Hill, R., Palmiéri, J., et al. (2019) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms001739 · Cited by 1,341 · see citing works
The imbalance of the Asian water tower
Yao, T., Bolch, T., Chen, D., Gao, J., Immerzeel, W. W., Piao, S. L., Su, F., Thompson, L. G., Wada, Y., Wang, L., et al. (2022) · Nature Reviews Earth & Environment · doi:10.1038/s43017-022-00299-4 · Cited by 1,299 · see citing works
Emissions – the ‘business as usual’ story is misleading
Hausfather, Z., & Peters, G. P. (2020) · Nature · doi:10.1038/d41586-020-00177-3 · Cited by 1,213 · see citing works
Harmonization of global land use change and management for the period 850–2100 (LUH2) for CMIP6
HURTT, G. C., Chini, L. P., Sahajpal, R., Frolking, S., Bodirsky, B. L., Calvin, K., Doelman, J., Fisk, J., Fujimori, S., Goldewijk, K. K., et al. (2020) · Geoscientific model development · doi:10.5194/gmd-13-5425-2020 · Cited by 1,283 · see citing works
Self-citationYukimoto, S., Kawai, H., Koshiro, T., Oshima, N., Yoshida, K., Urakawa, S., Tsujino, H., Deushi, M., Tanaka, T. Y., Hosaka, M., et al. (2019) · Journal of the Meteorological Society of Japan Ser II · doi:10.2151/jmsj.2019-051 · Cited by 1,217 · see citing works
(2019) · doi:10.5194/gmd-12-1443-2019 · Cited by 1,093 · see citing works
Self-citationClimate change increases cross-species viral transmission risk
Carlson, C. J., Albery, G. F., Merow, C., Trisos, C. H., Zipfel, C. M., Eskew, E. A., Olival, K. J., Ross, N., & Bansal, S. (2022) · Nature · doi:10.1038/s41586-022-04788-w · Cited by 1,099 · see citing works
The global methane budget 2000–2012
Saunois, M., Bousquet, P., Poulter, B., Peregon, A. M., Ciais, P., Canadell, J. G., Dlugokencky, E. J., Etiope, G., Bastviken, D., Houweling, S., et al. (2016) · Earth system science data · doi:10.5194/essd-8-697-2016 · Cited by 1,067 · see citing works
Self-citationTwenty‐First Century Drought Projections in the CMIP6 Forcing Scenarios
Cook, B. I., Mankin, J., Marvel, K., Williams, P., Smerdon, J. E., & Anchukaitis, K. J. (2020) · Earth s Future · doi:10.1029/2019ef001461 · Cited by 1,047 · see citing works
“We downloaded diagnostic output from climate models in the CMIP6 database (https://esgf-node.llnl.gov/ search/cmip6/), using the “historical” (1850–2014) simulations conducted as part of the core DECK experiments (Eyring et al., 2016) and four SSPs (2015–2100) from ScenarioMIP (O'Neill et al., 2016).”
MethodInfluentialEutrophication will increase during the 21st century as a result of precipitation changes
Sinha, E., Michalak, A. M., & Balaji, V. (2017) · Science · doi:10.1126/science.aan2409 · Cited by 1,028 · see citing works
Climate impacts on global agriculture emerge earlier in new generation of climate and crop models
Jägermeyr, J., Müller, C., Ruane, A., Elliott, J., Balkovič, J., Castillo, O., Faye, B., Foster, I. T., Folberth, C., Franke, J., et al. (2021) · Nature Food · doi:10.1038/s43016-021-00400-y · Cited by 903 · see citing works
Dunne, J. P. P., Horowitz, L. W., Adcroft, A., Ginoux, P. A., Held, I. M., John, J. G., Krasting, J. P., Malyshev, S. L., Naïk, V., Paulot, F., et al. (2020) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms002015 · Cited by 995 · see citing works
Seland, Ø., Bentsen, M., Olivié, D., Toniazzo, T., Gjermundsen, A., Graff, L. S., Debernard, J. B., Gupta, A. K., He, Y., Kirkevåg, A., et al. (2020) · Geoscientific model development · doi:10.5194/gmd-13-6165-2020 · Cited by 1,066 · see citing works
High-resolution (1 km) Köppen-Geiger maps for 1901–2099 based on constrained CMIP6 projections
Beck, H. E., McVicar, T. R., Vergopolan, N., Berg, A., Lutsko, N. J., Dufour, A., Zeng, Z., Jiang, X. S., van Dijk, A. I. J. M., & Miralles, D. G. (2023) · Scientific Data · doi:10.1038/s41597-023-02549-6 · Cited by 1,036 · see citing works
Séférian, R., Nabat, P., Michou, M., Saint‐Martin, D., Voldoire, A., Colin, J., Decharme, B., Delire, C., Berthet, S., Chevallier, M., et al. (2019) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms001791 · Cited by 925 · see citing works
“Finally, the current study documents the main characteristics and behavior of CNRM models over the CMIP6 Diagnostic, Evaluation and Characterization of Klima (DECK), CMIP6 historical, and the ScenarioMIP future projections.”
MethodInfluentialKwiatkowski, L., Torres, O., Bopp, L., Aumont, O., Chamberlain, M., Christian, J. R., Dunne, J. P., Gehlen, M., Ilyina, T., John, J. G., et al. (2020) · Biogeosciences · doi:10.5194/bg-17-3439-2020 · Cited by 897 · see citing works
Global projections of future urban land expansion under shared socioeconomic pathways
Chen, G., Li, X., Liu, X., Chen, Y., Liang, X., Leng, J., Xu, X., Liao, W., Qiu, Y., Wu, Q., et al. (2020) · Nature Communications · doi:10.1038/s41467-020-14386-x · Cited by 878 · see citing works
Climate model projections from the Scenario Model Intercomparison Project (ScenarioMIP) of CMIP6
Tebaldi, C., Debeire, K., Eyring, V., Fischer, E., Fyfe, J., Friedlingstein, P., Knutti, R., Lowe, J., O'Neill, B., Sanderson, B., et al. (2020) · Earth System Dynamics · doi:10.5194/esd-12-253-2021 · Cited by 736 · see citing works
“ScenarioMIP experiments and participating models As described in detail in O’Neill et al. (2016) and summarized in the matrix display of Fig.”
MethodSelf-citationNotz, D., & Community, S. (2020) · Geophysical Research Letters · doi:10.1029/2019gl086749 · Cited by 752 · see citing works
Historical greenhouse gas concentrations for climate modelling (CMIP6)
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Global field observations of tree die-off reveal hotter-drought fingerprint for Earth’s forests
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Thermal bottlenecks in the life cycle define climate vulnerability of fish
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Partitioning climate projection uncertainty with multiple large ensembles and CMIP5/6
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Self-citationThe Australian Earth System Model: ACCESS-ESM1.5
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The Detection and Attribution Model Intercomparison Project (DAMIP v1.0) contribution to CMIP6
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Self-citationAchievements and needs for the climate change scenario framework
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Self-citationProjected land ice contributions to twenty-first-century sea level rise
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Ubiquity of human-induced changes in climate variability
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“5 is a high emissions “fossil‐fueled development” scenario (O'Neill et al., 2016).”
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Projected Change in Temperature and Precipitation Over Africa from CMIP6
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The Decadal Climate Prediction Project (DCPP) contribution to CMIP6
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Global Methane Budget 2000–2020
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CMIP6 Simulations With the CMCC Earth System Model (CMCC‐ESM2)
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“In all future scenarios both carbon and nitrogen aggregated pools are characterized by an increase up to 2100, with extremes values reached by the ssp126 and ssp370 scenarios, which are respectively distinguished by maximum afforestation and deforestation interventions (O'Neill et al., 2016).”
BackgroundMethodInsight from CMIP6 SSP-RCP scenarios for future drought characteristics in China
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“Firstly, we apply the GCAM-China model to simulate China’s future energy and socioeconomic evolution under China’s national carbon neutrality goals and a family of climate-socioeconomic scenarios within CMIP6 [27,28].”
BackgroundMethodInfluentialAdded value of CMIP6 over CMIP5 models in simulating Indian summer monsoon rainfall
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Ice Sheet Model Intercomparison Project (ISMIP6) contribution to CMIP6
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“The future in CMIP6 falls under the guidance of ScenarioMIP (O’Neill et al., 2016), ISMIP6 will focus on the high-emission 20 scenario ssp585 that produces a radiative forcing of 8.”
InfluentialThe Mediterranean climate change hotspot in the CMIP5 and CMIP6 projections
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AerChemMIP: quantifying the effects of chemistry and aerosols in CMIP6
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Self-citationAntarctic Sea Ice Area in CMIP6
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“1 in the context of the CMIP6 DECK, historical simulations, and the ssp585 future scenario, which is a tier 1 experiment of the ScenarioMIP (O’Neill et al., 2016).”
BackgroundMethodInfluentialSelf-citationChanges in Annual Extremes of Daily Temperature and Precipitation in CMIP6 Models
Li, C., Zwiers, F., Zhang, X.-B., Li, G.-L., Sun, Y., & Wehner, M. (2020) · Journal of Climate · doi:10.1175/jcli-d-19-1013.1 · Cited by 309 · see citing works
CMIP6 Evaluation and Projection of Temperature and Precipitation over China
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Comparison of CMIP6 and CMIP5 models in simulating climate extremes
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“The models in CMIP6 generally have finer resolution with improved dynamical processes, and the new Shared Socioeconomic Pathway (SSP)/RCP-based emission scenarios are applied for future climate change simulations [12,13].”
MethodSmith, D. M., Screen, J. A., Deser, C., Cohen, J. L., Fyfe, J. C., García‐Serrano, J., Jung, T. J., Катцов, В. М., Matei, D., Msadek, R., et al. (2019) · Geoscientific model development · doi:10.5194/gmd-12-1139-2019 · Cited by 360 · see citing works
“In particular, the magnitudes of polar amplification simulated by different models in response to future and past radiative forcings will be assessed from Scenario MIP (O'Neill et al. 2016) and Paleoclimate MIP (Kageyama et al. 2016).”
Widespread shift from ecosystem energy to water limitation with climate change
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Insights From CMIP6 for Australia's Future Climate
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“This study uses one simulation each from up to 32 CMIP6 models that are available at the time of writing (Table 1), with most models having Historical simulations available for evaluation purposes and fewer models available for ScenarioMIP.”
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Self-citationGlobal climate-related predictors at kilometer resolution for the past and future
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Does CMIP6 Inspire More Confidence in Simulating Climate Extremes over China?
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Historical and future changes in air pollutants from CMIP6 models
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The 2021 western North America heat wave among the most extreme events ever recorded globally
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“M. Wehner, P. Gleckler, J. Lee, Characterization of long period return values of extreme daily temperature and precipitation in the CMIP6 models: Part 1, model evaluation.”
BackgroundMethodInfluentialGlobal energy growth is outpacing decarbonization
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“Zheng B (2018) Global Energy Growth Is Outpacing Decarbonization.”
BackgroundProjected Future Changes in Tropical Cyclones Using the CMIP6 HighResMIP Multimodel Ensemble
Roberts, M. J., Bellucci, A., Vannière, B., Camp, J., Roberts, C. D., Putrasahan, D. A., Mecking, J., Hodges, K., Terray, L., Caron, L., et al. (2020) · Geophysical Research Letters · doi:10.1029/2020gl088662 · Cited by 298 · see citing works
Making climate projections conditional on historical observations
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Seasonal Arctic sea ice forecasting with probabilistic deep learning
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Constraining the increased frequency of global precipitation extremes under warming
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Global water use efficiency saturation due to increased vapor pressure deficit
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Tong, D., Cheng, J., Liu, Y., et al. (2020) · Atmospheric chemistry and physics · doi:10.5194/acp-20-5729-2020 · Cited by 285 · see citing works
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“A set of future land-only time slice simulations (2015–2100) will be generated via forcing data obtained from at least 2 future climate scenarios from the ScenarioMIP (O’Neill et al., 2016) and will be executed at a later stage during CMIP6.”
Implementation of U.K. Earth System Models for CMIP6
Sellar, A., Walton, J. P. R. B., Jones, C., Wood, R., Abraham, N. L., Andrejczuk, M., Andrews, M. B., Andrews, T., Archibald, A. T., de Mora, L., et al. (2020) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2019ms001946 · Cited by 284 · see citing works
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Increased occurrence of high impact compound events under climate change
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Global surface air temperatures in CMIP6: historical performance and future changes
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“5 and O'Neill et al., 2016, for a description of the relationship between RCP4.”
BackgroundTropical cyclone climatology change greatly exacerbates US extreme rainfall–surge hazard
Gori, A., Lin, N., Xi, D., & Emanuel, K. (2022) · Nature Climate Change · doi:10.1038/s41558-021-01272-7 · Cited by 282 · see citing works
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James, R., Washington, R., Schleussner, C., Rogelj, J., & Conway, D. (2017) · Wiley Interdisciplinary Reviews Climate Change · doi:10.1002/wcc.457 · Cited by 271 · see citing works
“This additional RCP could facilitate 59 and so the number of GCM experiments will depend on the interest of the individual modeling centers.”
BackgroundAlmazroui, M., Ashfaq, M., Islam, M. N., Rashid, I. U., Kamil, S., Abid, M. A., O'Brien, E. W., Ismail, M., Reboita, M. S., Sörensson, A. A., et al. (2021) · Earth Systems and Environment · doi:10.1007/s41748-021-00233-6 · Cited by 267 · see citing works
“In the latest 6th phase of CMIP (CMIP6, O’Neill, 2016; Petrie et al.”
BackgroundConstraining human contributions to observed warming since the pre-industrial period
Gillett, N. P., Kirchmeier-Young, M., Ribes, A., Shiogama, H., Hegerl, G. C., Knutti, R., Gastineau, G., John, J. G., Li, L., Nazarenko, L., et al. (2021) · Nature Climate Change · doi:10.1038/s41558-020-00965-9 · Cited by 265 · see citing works
Self-citationUnderstanding Future Change of Global Monsoons Projected by CMIP6 Models
Wang, B., Jin, C., & Liu, J. (2020) · Journal of Climate · doi:10.1175/jcli-d-19-0993.1 · Cited by 226 · see citing works
Future drought characteristics through a multi-model ensemble from CMIP6 over South Asia
Zhai, J., Mondal, S. K., Fischer, T., Wang, Y., Su, B., Huang, J., Tao, H., Wang, G., Ullah, W., & Uddin, M. J. (2020) · Atmospheric Research · doi:10.1016/j.atmosres.2020.105111 · Cited by 265 · see citing works
Nijsse, F. J. M. M., Cox, P. M., & Williamson, M. S. (2020) · Earth System Dynamics · doi:10.5194/esd-11-737-2020 · Cited by 258 · see citing works
Xu, H., Yue, C., Zhang, Y., Liu, D., & Piao, S. (2023) · Proceedings of the National Academy of Sciences of the United States of America · doi:10.1073/pnas.2304988120 · Cited by 241 · see citing works
“The CO 2 fertilization effects on biomass were based on the results of model experiments (i.e., 1pctCO 2 experiments) carried out as part of the CMIP6 (33).”
InfluentialGlobal Land Monsoon Precipitation Changes in CMIP6 Projections
Chen, Z., Zhou, T., Zhang, L., Chen, X., Zhang, W., & Jiang, J. (2020) · Geophysical Research Letters · doi:10.1029/2019gl086902 · Cited by 252 · see citing works
He, C., Kim, H., Hashizume, M., Lee, W., Honda, Y., Kim, S. E., Kinney, P. L., Schneider, A. E., Zhang, Y., Zhu, Y., et al. (2022) · The Lancet Planetary Health · doi:10.1016/s2542-5196(22)00139-5 · Cited by 260 · see citing works
Understanding responses to climate-related water scarcity in Africa
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Compiled records of carbon isotopes in atmospheric CO 2 for historical simulations in CMIP6
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“In a separate paper, we will provide atmospheric Δ14C and δ13C for future scenarios in CMIP6 created with a simple carbon cycle model (Graven, 2015) and CO2 emission and concentration scenarios from ScenarioMIP (O'Neill et al., 2016).”
MethodRegional Climate Sensitivity of Climate Extremes in CMIP6 Versus CMIP5 Multimodel Ensembles
Seneviratne, S. I., & Hauser, M. (2020) · Earth s Future · doi:10.1029/2019ef001474 · Cited by 242 · see citing works
“In CMIP6, we combine the historical simulations (1850 to 2015) with the shared socioeconomic pathways (SSPs) projections (O'Neill et al., 2016) for the years 2016 to 2100.”
MethodAbyssal ocean overturning slowdown and warming driven by Antarctic meltwater
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Fertilizer management for global ammonia emission reduction
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Changing Lengths of the Four Seasons by Global Warming
Wang, J., Guan, Y., Wu, L., Guan, X., Cai, W., Huang, J., Dong, W., & Zhang, B. (2021) · Geophysical Research Letters · doi:10.1029/2020gl091753 · Cited by 248 · see citing works
- Authors
- O'Neill, B. C., Tebaldi, C., van Vuuren, D. P., Eyring, V., Friedlingstein, P., Hurtt, G., Knutti, R., Kriegler, E., Lamarque, J.-F., Lowe, J., Meehl, G. A., Moss, R., Riahi, K., & Sanderson, B. M.
- Affiliations
- NSF National Center for Atmospheric Research (US)
- Deutsches Zentrum für Luft- und Raumfahrt e. V. (DLR) (DE)
- University of Exeter (GB)
- University of Maryland, College Park (US)
- ETH Zurich (CH)
- Potsdam Institute for Climate Impact Research (DE)
- Met Office (GB)
- Joint Global Change Research Institute (US)
- International Institute for Applied Systems Analysis (AT)
- Corresponding author
- Tebaldi, Claudia
- Eyring, Veronika
- Friedlingstein, Pierre
- Hurtt, George
- Knutti, Reto
- Kriegler, Elmar
- Lowe, Jason
- Meehl, Gerald A.
- Moss, Richard
- Riahi, Keywan
- Sanderson, Benjamin M.
- ORCID
- Venue
- Geoscientific Model Development
- Publisher
- Copernicus GmbH
- Published
- 2016-09-28
- Volume
- 9
- Issue
- 9
- Pages
- 3461-3482
- ISSN
- 1991-959X (ISSN-L)
- 1991-9603
- OpenAlex
- W2337225114
- Semantic Scholar
- f71367b378592324c4f7aed362e542e4c901a111
- Cited by
- 5,241
- References
- 72
- Citations by year
- 2026: 835 · 2025: 1024 · 2024: 974 · 2023: 897 · 2022: 727 · 2021: 480 · 2020: 206 · 2019: 48 · 2018: 18 · 2017: 13 · 2016: 15 · 2014: 1
- FWCI
- 23.13
- Type
- journal article
- Language
- en
- Open access
- gold
- doi.org
- Licence
- Locations
- Geoscientific model development (publishedVersion, cc-by)
- IIASA PURE (International Institute of Applied Systems Analysis) (acceptedVersion)
- elib (German Aerospace Center) (submittedVersion)
- OSTI OAI (U.S. Department of Energy Office of Scientific and Technical Information) (submittedVersion)
- DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion, cc-by-sa)
- Utrecht University Repository (Utrecht University) (submittedVersion, other-oa)
- Figshare (submittedVersion)
- RENATE (submittedVersion, cc-by-nc-nd)
- Open Research Exeter (University of Exeter) (submittedVersion, cc-by)
- Publication Database PIK (Potsdam Institute for Climate Impact Research (PIK)) (submittedVersion, other-oa)
- Repository for Publications and Research Data (ETH Zurich) (submittedVersion, cc-by)
- RENATE (cc-by)
- ETH Zürich Research Collection (cc-by)
- Funders
- U.S. Department of Energy (DEFC0297ER62402, FC02-97ER62402)
- European Commission (641816, HORIZON2020)
- Office of Science (FC02-97ER62402, Cooperative Agreement DE-FC02-97ER62402, DEFC0297ER62402)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Social Sciences › Economics, Econometrics and Finance › Economics and Econometrics › Climate Change Policy and Economics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate Change and Geoengineering
- Keywords
- ScenarioMIP, CMIP6, climate change projections, emission scenarios, land use change, integrated assessment models, multi-model intercomparison, scenario-based assessment, 2 °C warming limit, long-term climate projections, natural climate variability, IPCC assessment
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Claims read by deepseek-v4.1-flash under definition version 3 (extract-v3) on 2026-10-16.
Classified by jev-1.13-20260917 (gold-guideline-v0.2) on 2026-10-16.
Cited sources are checked by gpt-6-sol.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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