文献类型：期刊文献

英文题名：Differential expansion speeds of Indo-Pacific warm pool and deep convection favoring pool under greenhouse warming

作者：Leung, Jeremy Cheuk-Hin[1];Zhang, Banglin[1,2,3];Gan, Qiuying[1,4];Wang, Lei[4];Qian, Weihong[1,5];Hu, Zeng-Zhen[6]

机构：[1]CMA, Guangdong Prov Key Lab Reg Numer Weather Predict, Guangzhou Inst Trop & Marine Meteorol, Guangzhou, Peoples R China;[2]Lanzhou Univ, Coll Atmospher Sci, Lanzhou, Peoples R China;[3]Southern Marine Sci & Engn Guangdong Lab, Zhuhai, Peoples R China;[4]Guangdong Ocean Univ, Coll Ocean & Meteorol, Lab Coastal Ocean Variat & Disaster Predict, Zhanjiang, Peoples R China;[5]Peking Univ, Dept Atmospher & Ocean Sci, Beijing, Peoples R China;[6]NOAA, Climate Predict Ctr, NCEP, NWS, 5830 Univ Res Court, College Pk, MD 20740 USA

年份：2022

卷号：5

期号：1

外文期刊名：NPJ CLIMATE AND ATMOSPHERIC SCIENCE

收录：SCI-EXPANDED(收录号：WOS:000888740100001)、、Scopus(收录号：2-s2.0-85142495044)、WOS

基金：This work is supported by the Guangdong Province Introduction of Innovative R&D Team Project China (2019ZT08G669), the Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), the Guangdong Basic and Applied Basic Research Foundation (2020A1515110275), the National Natural Science Foundation of China (41776031).

语种：英文

外文摘要：The Indo-Pacific warm pool (IPWP), which affects the global climate system through supporting tropical convection, has been reported to expand significantly under greenhouse warming. Although early research revealed that the sea surface temperature (SST) threshold for deep convection (sigma(conv)) increases with global warming, many latest relevant works were still conducted based on the traditional IPWP definition (e.g., static SST= 28 degrees C threshold, and is referred to as the oceanic warm pool, OWP28). Here, we claim that the OWP28 expansion differs from the deep convection favoring pool (DCFP) area change and may not reflect the direct impacts of Indo-Pacific warming on the climate system. Results show that, because of the long-term increase in sigma(conv), the DCFP expands at a rate 2.6 times slower than the OWP28 from 1979 to 2020. The difference reaches 12-27 times from 2015-2100 under different emission scenarios, based on CMIP6 model simulations. While the OWP28 expands to the eastern Pacific, the DCFP will remain within the Indian Ocean and western Pacific Ocean regardless of emission levels. This study emphasizes the necessity of considering the response of the relationship between deep convection and SST to climate change when studying the long-term variability of the IPWP.