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Abstract
The Coupled Model Intercomparison Project (phase 6) (CMIP6) global circulation models
(GCMs) predict equilibrium climate sensitivity (ECS) values ranging between 1.8 and
5.7
∘
C. To narrow this range, we group 38 GCMs into low, medium and high ECS subgroups
and test their accuracy and precision in hindcasting the mean global surface warming
observed from 1980–1990 to 2011–2021 in the ERA5-T2m, HadCRUT5, GISTEMP v4, and NOAAGlobTemp
v5 global surface temperature records. We also compare the GCM hindcasts to the satellite-based
UAH-MSU v6 lower troposphere global temperature record. We use 143 GCM ensemble averaged
simulations under four slightly different forcing conditions, 688 GCM member simulations,
and Monte Carlo modeling of the internal variability of the GCMs under three different
model accuracy requirements. We found that the medium and high-ECS GCMs run too hot
up to over 95% and 97% of cases, respectively. The low ECS GCM group agrees best with
the warming values obtained from the surface temperature records, ranging between
0.52 and 0.58
∘
C. However, when comparing the observed and GCM hindcasted warming on land and ocean
regions, the surface-based temperature records appear to exhibit a significant warming
bias. Furthermore, if the satellite-based UAH-MSU-lt record is accurate, actual surface
warming from 1980 to 2021 may have been around 0.40
∘
C (or less), that is up to about 30% less than what is reported by the surface-based
temperature records. The latter situation implies that even the low-ECS models would
have produced excessive warming from 1980 to 2021. These results suggest that the
actual ECS may be relatively low, i.e. lower than 3
∘
C or even less than 2
∘
C if the 1980–2021 global surface temperature records contain spurious warming, as
some alternative studies have already suggested. Therefore, the projected global climate
warming over the next few decades could be moderate and probably not particularly
alarming.
By coordinating the design and distribution of global climate model simulations of the past, current, and future climate, the Coupled Model Intercomparison Project (CMIP) has become one of the foundational elements of climate science. However, the need to address an ever-expanding range of scientific questions arising from more and more research communities has made it necessary to revise the organization of CMIP. After a long and wide community consultation, a new and more federated structure has been put in place. It consists of three major elements: (1) a handful of common experiments, the DECK (Diagnostic, Evaluation and Characterization of Klima) and CMIP historical simulations (1850–near present) that will maintain continuity and help document basic characteristics of models across different phases of CMIP; (2) common standards, coordination, infrastructure, and documentation that will facilitate the distribution of model outputs and the characterization of the model ensemble; and (3) an ensemble of CMIP-Endorsed Model Intercomparison Projects (MIPs) that will be specific to a particular phase of CMIP (now CMIP6) and that will build on the DECK and CMIP historical simulations to address a large range of specific questions and fill the scientific gaps of the previous CMIP phases. The DECK and CMIP historical simulations, together with the use of CMIP data standards, will be the entry cards for models participating in CMIP. Participation in CMIP6-Endorsed MIPs by individual modelling groups will be at their own discretion and will depend on their scientific interests and priorities. With the Grand Science Challenges of the World Climate Research Programme (WCRP) as its scientific backdrop, CMIP6 will address three broad questions: – How does the Earth system respond to forcing? – What are the origins and consequences of systematic model biases? – How can we assess future climate changes given internal climate variability, predictability, and uncertainties in scenarios? This CMIP6 overview paper presents the background and rationale for the new structure of CMIP, provides a detailed description of the DECK and CMIP6 historical simulations, and includes a brief introduction to the 21 CMIP6-Endorsed MIPs.
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