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      From a Spatial Structure Perspective: Spatial‐Temporal Variation of Climate Redistribution of China Based on the Köppen–Geiger Classification

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          Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization

          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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            Nonparametric Tests Against Trend

            Henry Mann (1945)
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              Updated world map of the Köppen-Geiger climate classification

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                Author and article information

                Contributors
                Journal
                Geophysical Research Letters
                Geophysical Research Letters
                American Geophysical Union (AGU)
                0094-8276
                1944-8007
                August 16 2022
                August 08 2022
                August 16 2022
                : 49
                : 15
                Affiliations
                [1 ]School of Environmental Science and Engineering Southern University of Science and Technology Shenzhen China
                [2 ]Department of Civil and Environmental Engineering University of Connecticut Storrs CT USA
                [3 ]Key Laboratory of Water Cycle and Related Land Surface Process Institute of Geographic Science and Natural Resources Research Chinese Academy of Science Beijing China
                [4 ]Department of Geosciences and Geography University of Helsinki Helsinki Finland
                [5 ]Institute for Atmospheric and Earth System Research, Faculty of Science University of Helsinki Helsinki Finland
                Article
                10.1029/2022GL099319
                a1f63d59-0819-4a27-973f-26950158a983
                © 2022

                http://creativecommons.org/licenses/by-nc/4.0/

                http://doi.wiley.com/10.1002/tdm_license_1.1

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