期刊
ENVIRONMENTAL RESEARCH LETTERS
卷 18, 期 3, 页码 -出版社
IOP Publishing Ltd
DOI: 10.1088/1748-9326/acb836
关键词
precipitation extremes; Clausius-Clapeyron relation; precipitation duration; hook structure; climate change
Global warming has significantly impacted precipitation extremes by altering the energy budget and water cycle of the land-atmosphere system. This study quantifies the global-scale responses of precipitation extremes to near-surface air temperature and dew point temperature using the ERA5 reanalysis dataset. The results reveal a "hook" structure between precipitation extremes and temperature, with various factors influencing this relationship.
Global warming has altered the energy budget and water cycle processes of the land-atmosphere system, which has resulted in significant effects on precipitation extremes. Previous studies have identified a hook structure between near-surface temperature and precipitation extremes, in which extremes increase with temperature rises and decline thereafter. However, the underlying physical mechanisms of this association remain poorly understood. In this study, global-scale responses of precipitation extremes to near-surface air temperature (SAT) and dew point temperature (DPT) were quantified using the ERA5 reanalysis dataset. The results reveal a hook structure between precipitation extremes scaling and temperature, for both SAT and DPT, over many regions worldwide. The peak point temperature (T (pp)) ranges from 15 degrees C to 25 degrees C, increasing as latitude decreased. The association of precipitation extremes with SAT is negative in many areas in the tropics, whereas that with DPT is almost always positive; this suggests that moisture supply is the main factor limiting precipitation at higher surface temperatures. The hook structure and scaling rates incompatible with Clausius-Clapeyron scaling are associated with various factors including precipitation duration, total column water vapour, convective available potential energy, and relative humidity.
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