Will the 2022 compound heatwave-drought extreme over the Yangtze River Basin become Grey Rhino in the future?OA
Will the 2022 compound heatwave-drought extreme over the Yangtze River Basin become Grey Rhino in the future?
The increasingly frequent and severe regional-scale compound heatwave-drought extreme events(CHDEs),driven by global warming,present formidable challenges to ecosystems,residential livelihoods,and economic conditions.However,uncertainty persists regarding the future trend of CHDEs and their insights into regional spatiotemporal heterogeneity.By integrating daily meteorological data from observations in 1961-2022 and global climate models(GCMs)based on the Shared Socioeconomic Pathways,the evolution patterns of CHDEs were compared and examined among three sub-catchments of the Yangtze River Basin,and the return periods of CHDE in 2050s and 2100s were projected.The findings indicate that the climate during the 2022 CHDE period was the warmest and driest recorded in 1961-2022,with precipitation less than 154.5 mm and a mean daily maximum temperature 3.4 ℃ higher than the average of 1981-2010,whereas the char-acteristics in the sub-catchments exhibited temporal and spatial variation.In July-August 2022,the most notable feature of CHDE was its extremeness since 1961,with return periods of~200-year in upstream,80-year in midstream,and 40-year in downstream,respectively.By 2050,the return periods witnessed 2022 CHDE would likely be reduced by one-third.Looking towards 2100,under the highest emission scenario of SSP585,it was projected to substantially increase the frequency of CHDEs,with return periods reduced to one-third in the upstream and downstream,as well as halved in the midstream.These findings provide valuable insights into the changing risks associated with forthcoming climate extremes,emphasizing the urgency of addressing these challenges in regional management and sustainable development.
Ai-Qing FENG;Qing-Chen CHAO;Lu-Lu LIU;Ge GAO;Guo-Fu WANG;Xue-Jun ZHANG;Qi-Guang WANG
China Meteorological Administration Key Laboratory for Climate Prediction Studies,National Climate Centre,Beijing 100081,ChinaKey Laboratory of Land Surface Pattern and Simulation,Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences,Beijing 100101,ChinaChina Institute of Water Resources and Hydropower Research,Beijing 100038,ChinaChina Meteorological Administration Training Centre,China Meteorological Administration,Beijing 100081,China
Compound extreme eventJoint return periodDroughtHeatwaveClimate changeYangtze River Basin
《气候变化研究进展(英文版)》 2024 (003)
547-556 / 10
The authors acknowledged the National Natural Science Foundation of China(42371084,42101311,41975100),the Special Project for Compilation of the Fourth National Assessment Report on Climate Change of the Ministry of Science and Technology(210YBXM2018108002),the Youth Open Project of China Meteorological Administration Key Laboratory for Climate Prediction Studies(CMA-LCPS-23-04),the Innovation and Development Project of China Mete-orological Administration(CXFZ2024J037),and the China Yangtze Power Co.,Ltd(Z242302014).In addition,the au-thors would like to ex press sincere gratitude to the editor and anonymous reviewers for their invaluable feedback and constructive suggestions,whose expertise and insights greatly contributed to the improvement of this study.
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