Global Change in Agricultural Flash Drought over the 21st Century  

作　　者：Emily BLACK 

机构地区：[1]National Centre for Atmospheric Science,Fairbairn House,71-75 Clarendon Road,Leeds,LS29PH,U.K [2]Department of Meteorology,Brian Hoskins Building,University of Reading,Whiteknights campus,Reading,RG66ET,U.K.

出　　处：《Advances in Atmospheric Sciences》2024年第2期209-220,I0002-I0019,共30页大气科学进展（英文版）

基　　金：supported by the National Centre for Atmospheric Science through the NERC National Capability International Programmes Award (NE/ X006263/1);the Global Challenges Research Fund, via Atmospheric hazard in developing Countries: Risk assessment and Early Warning (ACREW) (NE/R000034/1);the Natural Environmental Research Council and the Department for Foreign International Development through the Sat WIN-ALERT project (NE/ R014116/1)。

摘　　要：Agricultural flash droughts are high-impact phenomena, characterized by rapid soil moisture dry down. The ensuing dry conditions can persist for weeks to months, with detrimental effects on natural ecosystems and crop cultivation. Increases in the frequency of these rare events in a future warmer climate would have significant societal impact. This study uses an ensemble of 10 Coupled Model Intercomparison Project(CMIP) models to investigate the projected change in agricultural flash drought during the 21st century. Comparison across geographical regions and climatic zones indicates that individual events are preceded by anomalously low relative humidity and precipitation, with long-term trends governed by changes in temperature, relative humidity, and soil moisture. As a result of these processes, the frequency of both upperlevel and root-zone flash drought is projected to more than double in the mid-and high latitudes over the 21st century, with hot spots developing in the temperate regions of Europe, and humid regions of South America, Europe, and southern Africa.

关 键 词：flash drought climate change soil moisture agricultural drought CMIP 

分 类 号：S423[农业科学—植物保护]