Extreme characteristics and causes of the drought event in the whole Yangtze River Basin in the midsummer of 2022

IF 6.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES
Zhuo-Zhuo Lyu , Hui Gao , Rong Gao , Ting Ding
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引用次数: 1

Abstract

Due to their huge socio-economic impacts and complex formation causes, extreme and continuous drought events have become the focus and nodus of research in recent years. In the midsummer (July–August) of 2022, a severe drought event occurred in the whole Yangtze River Basin (YRB), China. During that period, the precipitation in the upper, middle and lower reaches of the YRB dropped over 40% less than the 1961–2021 climatic mean, which had never happened previously. Furthermore, the temperature was the highest during 1961–2022. The record-breaking magnitude of less rainfall and high temperature directly led to the continuous development of this extreme drought event. An atmospheric moisture budget analysis revealed that the YRB midsummer rainfall anomaly was dominated by the anomalous powerful vertical moisture advection, which was derived from the strongest descending motion over the whole YRB in the 2022 midsummer during 1981–2022. The western Pacific subtropical high (WPSH) during the midsummer remained stronger, more westward and lasted longer than the climatic mean. As a result, the whole YRB was controlled by a positive geopotential height centre. Further evidence revealed that the anomalous subtropical zonal flow played a crucial role in inducing the extreme descent over the YRB. Moreover, the anomalous upper-tropospheric easterly flow over the YRB in 2022 is the strongest during 1981–2022, modulating the generation of the unprecedented descent anomaly over the YRB. The likelihood that an integrated connection of severe drought in East Asia and flood in West Asia and northwestern South Asia would increase when the extremely strong easterly anomalies in the upper troposphere emerged and induced descending adiabatic flow on the eastern sides of the Tibetan Plateau. The results of this study can provide scientific insights into the predictability of extreme drought events and provide ways to improve predictions.

2022年盛夏全长江流域干旱事件的极端特征及成因
极端持续干旱事件由于其巨大的社会经济影响和复杂的形成原因,成为近年来研究的热点和难点。2022年盛夏(7 - 8月),中国长江流域发生了一次严重干旱事件。在此期间,长江上游、中下游降水比1961—2021年的气候平均值减少了40%以上,这是前所未有的。其中1961-2022年的气温最高。破纪录的少雨和高温直接导致了这次极端干旱事件的持续发展。大气水汽收支分析结果表明,青藏高原2022年盛夏降水异常主要由异常的强垂直水汽平流主导,该平流来源于整个青藏高原最强的下降运动。盛夏期间西太平洋副热带高压(WPSH)偏强、偏西、持续时间较气候平均值长。因此,整个YRB由一个正的位势高度中心控制。进一步的证据表明,副热带纬向异常气流在诱发青藏高原极端下降过程中发挥了重要作用。此外,2022年YRB上空对流层上层偏东气流异常在1981-2022年最强,调节了YRB上空前所未有的下降异常的产生。当对流层上层出现极强的偏东风异常,并在青藏高原东侧诱发下行绝热流时,东亚严重干旱与西亚和南亚西北部洪水综合联系的可能性增加。本研究的结果可以为极端干旱事件的可预测性提供科学的见解,并提供改进预测的方法。
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来源期刊
Advances in Climate Change Research
Advances in Climate Change Research Earth and Planetary Sciences-Atmospheric Science
CiteScore
9.80
自引率
4.10%
发文量
424
审稿时长
107 days
期刊介绍: Advances in Climate Change Research publishes scientific research and analyses on climate change and the interactions of climate change with society. This journal encompasses basic science and economic, social, and policy research, including studies on mitigation and adaptation to climate change. Advances in Climate Change Research attempts to promote research in climate change and provide an impetus for the application of research achievements in numerous aspects, such as socioeconomic sustainable development, responses to the adaptation and mitigation of climate change, diplomatic negotiations of climate and environment policies, and the protection and exploitation of natural resources.
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