{"has_accepted_license":"1","scopus_import":"1","intvolume":" 10","related_material":{"link":[{"description":"News on ISTA Website","relation":"press_release","url":"https://ista.ac.at/en/news/cloud-clustering-causes-more-extreme-rain/"}]},"user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","status":"public","article_number":"eadj6801","date_updated":"2024-03-05T09:26:47Z","ddc":["550"],"publication_status":"published","type":"journal_article","volume":10,"quality_controlled":"1","title":"Intensification of daily tropical precipitation extremes from more organized convection","article_processing_charge":"Yes","date_published":"2024-02-23T00:00:00Z","acknowledgement":"This work is supported by the Max-Planck-Gesellschaft (MPG). We greatly appreciate computational resources from Deutsches Klimarechenzentrum (DKRZ) and the Jülich Supercomputing Centre (JSC). ICONA/O simulations are funded through the NextGEMS project by the EU’s Horizon 2020 programme (grant agreement no. 101003470). ICONA simulations are funded through the MONSOON-2.0 project (grant agreement no. 01LP1927A) which is supported from German Federal Ministry of Education and Research (BMBF). J.B. acknowledges funding from the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant (grant agreement no. 101034413). B.S. acknowledges funding from the EU’s Horizon 2020 programme (grant agreement no. 101003470). C.M. gratefully acknowledges funding from the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation program (Project CLUSTER, grant agreement no. 805041).","doi":"10.1126/sciadv.adj6801","_id":"15047","publisher":"American Association for the Advancement of Science","external_id":{"pmid":["38394192"]},"date_created":"2024-03-03T23:00:50Z","file":[{"content_type":"application/pdf","file_name":"2024_ScienceAdv_Bao.pdf","relation":"main_file","date_updated":"2024-03-04T07:34:00Z","success":1,"access_level":"open_access","date_created":"2024-03-04T07:34:00Z","file_id":"15051","creator":"dernst","file_size":800926,"checksum":"d4ec4f05a6d14745057e14d1b8bf45ae"}],"oa":1,"file_date_updated":"2024-03-04T07:34:00Z","department":[{"_id":"CaMu"}],"project":[{"call_identifier":"H2020","grant_number":"101034413","_id":"fc2ed2f7-9c52-11eb-aca3-c01059dda49c","name":"IST-BRIDGE: International postdoctoral program"},{"_id":"629205d8-2b32-11ec-9570-e1356ff73576","name":"organization of CLoUdS, and implications of Tropical cyclones and for the Energetics of the tropics, in current and waRming climate","call_identifier":"H2020","grant_number":"805041"}],"month":"02","day":"23","article_type":"original","tmp":{"name":"Creative Commons Attribution 4.0 International Public License (CC-BY 4.0)","legal_code_url":"https://creativecommons.org/licenses/by/4.0/legalcode","image":"/images/cc_by.png","short":"CC BY (4.0)"},"pmid":1,"issue":"8","author":[{"id":"bb9a7399-fefd-11ed-be3c-ae648fd1d160","first_name":"Jiawei","last_name":"Bao","full_name":"Bao, Jiawei"},{"full_name":"Stevens, Bjorn","last_name":"Stevens","first_name":"Bjorn"},{"full_name":"Kluft, Lukas","last_name":"Kluft","first_name":"Lukas"},{"last_name":"Muller","full_name":"Muller, Caroline J","orcid":"0000-0001-5836-5350","first_name":"Caroline J","id":"f978ccb0-3f7f-11eb-b193-b0e2bd13182b"}],"language":[{"iso":"eng"}],"year":"2024","publication_identifier":{"eissn":["2375-2548"]},"ec_funded":1,"publication":"Science Advances","abstract":[{"lang":"eng","text":"Tropical precipitation extremes and their changes with surface warming are investigated using global storm resolving simulations and high-resolution observations. The simulations demonstrate that the mesoscale organization of convection, a process that cannot be physically represented by conventional global climate models, is important for the variations of tropical daily accumulated precipitation extremes. In both the simulations and observations, daily precipitation extremes increase in a more organized state, in association with larger, but less frequent, storms. Repeating the simulations for a warmer climate results in a robust increase in monthly-mean daily precipitation extremes. Higher precipitation percentiles have a greater sensitivity to convective organization, which is predicted to increase with warming. Without changes in organization, the strongest daily precipitation extremes over the tropical oceans increase at a rate close to Clausius-Clapeyron (CC) scaling. Thus, in a future warmer state with increased organization, the strongest daily precipitation extremes over oceans increase at a faster rate than CC scaling."}],"oa_version":"Published Version","citation":{"apa":"Bao, J., Stevens, B., Kluft, L., & Muller, C. J. (2024). Intensification of daily tropical precipitation extremes from more organized convection. Science Advances. American Association for the Advancement of Science. https://doi.org/10.1126/sciadv.adj6801","chicago":"Bao, Jiawei, Bjorn Stevens, Lukas Kluft, and Caroline J Muller. “Intensification of Daily Tropical Precipitation Extremes from More Organized Convection.” Science Advances. American Association for the Advancement of Science, 2024. https://doi.org/10.1126/sciadv.adj6801.","short":"J. Bao, B. Stevens, L. Kluft, C.J. Muller, Science Advances 10 (2024).","ama":"Bao J, Stevens B, Kluft L, Muller CJ. Intensification of daily tropical precipitation extremes from more organized convection. Science Advances. 2024;10(8). doi:10.1126/sciadv.adj6801","ista":"Bao J, Stevens B, Kluft L, Muller CJ. 2024. Intensification of daily tropical precipitation extremes from more organized convection. Science Advances. 10(8), eadj6801.","mla":"Bao, Jiawei, et al. “Intensification of Daily Tropical Precipitation Extremes from More Organized Convection.” Science Advances, vol. 10, no. 8, eadj6801, American Association for the Advancement of Science, 2024, doi:10.1126/sciadv.adj6801.","ieee":"J. Bao, B. Stevens, L. Kluft, and C. J. Muller, “Intensification of daily tropical precipitation extremes from more organized convection,” Science Advances, vol. 10, no. 8. American Association for the Advancement of Science, 2024."}}