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      Advancing research on compound weather and climate events via large ensemble model simulations

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          Abstract

          Societally relevant weather impacts typically result from compound events, which are rare combinations of weather and climate drivers. Focussing on four event types arising from different combinations of climate variables across space and time, here we illustrate that robust analyses of compound events — such as frequency and uncertainty analysis under present-day and future conditions, event attribution to climate change, and exploration of low-probability-high-impact events — require data with very large sample size. In particular, the required sample is much larger than that needed for analyses of univariate extremes. We demonstrate that Single Model Initial-condition Large Ensemble (SMILE) simulations from multiple climate models, which provide hundreds to thousands of years of weather conditions, are crucial for advancing our assessments of compound events and constructing robust model projections. Combining SMILEs with an improved physical understanding of compound events will ultimately provide practitioners and stakeholders with the best available information on climate risks.

          Abstract

          The authors show that robust analyses of high-impact compound weather and climate events require many samples. Thus, they argue that large ensemble climate model simulations should be used to provide the best available information on climate risks.

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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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            The next generation of scenarios for climate change research and assessment.

            Advances in the science and observation of climate change are providing a clearer understanding of the inherent variability of Earth's climate system and its likely response to human and natural influences. The implications of climate change for the environment and society will depend not only on the response of the Earth system to changes in radiative forcings, but also on how humankind responds through changes in technology, economies, lifestyle and policy. Extensive uncertainties exist in future forcings of and responses to climate change, necessitating the use of scenarios of the future to explore the potential consequences of different response options. To date, such scenarios have not adequately examined crucial possibilities, such as climate change mitigation and adaptation, and have relied on research processes that slowed the exchange of information among physical, biological and social scientists. Here we describe a new process for creating plausible scenarios to investigate some of the most challenging and important questions about climate change confronting the global community.
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              Uncertainty in climate change projections: the role of internal variability

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                Author and article information

                Contributors
                emanuele.bevacqua@ufz.de
                Journal
                Nat Commun
                Nat Commun
                Nature Communications
                Nature Publishing Group UK (London )
                2041-1723
                14 April 2023
                14 April 2023
                2023
                : 14
                : 2145
                Affiliations
                [1 ]GRID grid.7492.8, ISNI 0000 0004 0492 3830, Department of Computational Hydrosystems, , Helmholtz Centre for Environmental Research—UFZ, ; Leipzig, Germany
                [2 ]GRID grid.450268.d, ISNI 0000 0001 0721 4552, Max Planck Institute for Meteorology, ; Hamburg, Germany
                [3 ]GRID grid.5801.c, ISNI 0000 0001 2156 2780, Institute for Atmospheric and Climate Science, ETH Zurich, ; Zurich, Switzerland
                [4 ]GRID grid.4444.0, ISNI 0000 0001 2112 9282, Institut Pierre-Simon Laplace, CNRS, ; Paris, France
                [5 ]GRID grid.10877.39, ISNI 0000000121581279, LMD/IPSL, ENS, Université PSL, École Polytechnique, Institut Polytechnique de Paris, , Sorbonne Université, CNRS, Ecole des Ponts, ; Marne-la-Vallée, France
                [6 ]GRID grid.5386.8, ISNI 000000041936877X, Department of Earth and Atmospheric Sciences, , Cornell University, ; Ithaca, NY USA
                [7 ]GRID grid.57828.30, ISNI 0000 0004 0637 9680, Climate and Global Dynamics Laboratory, , National Center for Atmospheric Research, ; Boulder, CO USA
                [8 ]Polar Bears International, Bozeman, MT USA
                [9 ]GRID grid.460789.4, ISNI 0000 0004 4910 6535, Laboratoire des Sciences du Climat et de l’Environnement, IPSL, CEA-CNRS-UVSQ, , Université Paris-Saclay, ; Gif-sur-Yvette, France
                Author information
                http://orcid.org/0000-0003-0472-5183
                http://orcid.org/0000-0002-0008-5943
                http://orcid.org/0000-0003-4632-9701
                http://orcid.org/0000-0002-6176-0439
                http://orcid.org/0000-0001-8534-5355
                http://orcid.org/0000-0001-6045-1629
                Article
                37847
                10.1038/s41467-023-37847-5
                10104877
                37059735
                4141cd59-4c7f-461e-ad1c-b938e8cb4448
                © The Author(s) 2023

                Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

                History
                : 24 June 2022
                : 31 March 2023
                Funding
                Funded by: This project has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No 101003469. Funding was received by the European COST Action DAMOCLES (CA17109).
                Funded by: L.S.G. received funding from the German Ministry of Education and Research (BMBF) under the ClimXtreme project DecHeat (Grant number 01LP1901F) and from the European Union’s Horizon Europe Framework Programme under the Marie Skłodowska-Curie grant agreement No 101064940.
                Funded by: P.Y. is supported by the European Union’s Horizon 2020 research and innovation programme (grant agreement 101003469) and the French ANR (SAMPRACE project).
                Funded by: J.Z. acknowledges the Helmholtz Initiative and Networking Fund (Young Investigator Group COMPOUNDX, Grant Agreement VH-NG-1537).
                Categories
                Article
                Custom metadata
                © The Author(s) 2023

                Uncategorized
                projection and prediction,environmental sciences,natural hazards
                Uncategorized
                projection and prediction, environmental sciences, natural hazards

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