中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Response of evapotranspiration to the 2022 unprecedented extreme drought in the Yangtze River Basin

文献类型:期刊论文

作者Zhang, Yu1,2; Liu, Xiaomang2; Wang, Kaiwen2; Bai, Peng2
刊名INTERNATIONAL JOURNAL OF CLIMATOLOGY
出版日期2024-05-06
卷号N/A页码:13
关键词drought evapotranspiration extreme event in 2022 water balance Yangtze River Basin
ISSN号0899-8418
DOI10.1002/joc.8480
英文摘要The response of evapotranspiration (ET) to drought is essential for understanding water availability under drought conditions, which has received increasing scientific attention but remains highly uncertain. An unprecedented extreme drought sweeping the whole Yangtze River Basin during the summer and autumn of 2022 provides a novel opportunity to explore the ET response to drought within large river basins. Here, we apply multiple ET products to investigate the spatiotemporal variation of ET during the 2022 extreme drought and analyse the response of ET to drought in the Yangtze River Basin. The results show that this drought, characterized by widespread substantial precipitation deficit and high level of atmospheric evaporative demand (AED), leads to evident abnormal ET. Over the whole basin, ET exhibits a notable increase in the initial 2 months of this drought, which can significantly reduce water availability. However, despite continued high AED, the increase in ET fails to remain in the following months due to limited moisture supply. This suggests that ET response to drought varies as drought progresses. Among other drought events from 2003 to 2022, the response of ET is similar to that in the 2022 extreme drought. Specifically, for most sub-basins, ET typically shows positive anomalies in the early stage of drought, followed by negative anomalies in the late stage. Generally, our findings improve the understanding of the dynamic response of ET to drought at the basin scale, which is crucial for basin water security. During the 2022 unprecedented extreme drought in the Yangtze River Basin, evapotranspiration (ET) experienced a remarkable increase driven by high water demand initially, then a decline constrained by water supply. Among other drought events from 2003 to 2022, the response pattern of ET is similar to that in the 2022 extreme drought. image
WOS关键词GLOBAL LAND ; TERRESTRIAL EVAPORATION ; DATA ASSIMILATION ; WATER-BUDGET
资助项目National Key Research and Development Program of China ; [2023YFC3206600]
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:001214703200001
出版者WILEY
资助机构National Key Research and Development Program of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/204854]  
专题陆地水循环及地表过程院重点实验室_外文论文
通讯作者Liu, Xiaomang
作者单位1.Univ Chinese Acad Sci, Beijing, Peoples R China
2.Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Yu,Liu, Xiaomang,Wang, Kaiwen,et al. Response of evapotranspiration to the 2022 unprecedented extreme drought in the Yangtze River Basin[J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY,2024,N/A:13.
APA Zhang, Yu,Liu, Xiaomang,Wang, Kaiwen,&Bai, Peng.(2024).Response of evapotranspiration to the 2022 unprecedented extreme drought in the Yangtze River Basin.INTERNATIONAL JOURNAL OF CLIMATOLOGY,N/A,13.
MLA Zhang, Yu,et al."Response of evapotranspiration to the 2022 unprecedented extreme drought in the Yangtze River Basin".INTERNATIONAL JOURNAL OF CLIMATOLOGY N/A(2024):13.

入库方式: OAI收割

来源:地理科学与资源研究所

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