从两次不同极端事件看长江流域复合热干旱变化特征

IF 3.5 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
An Xuehua, Sun Shanlei, Ma Qianrong, Wu Hao, Li Daiyuan, Wu Wei
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引用次数: 0

摘要

复合热干旱事件对生态系统、农业和公共卫生产生深远影响,突出表明需要了解其特征和驱动机制,以制定有效的气候变化减缓和适应战略。研究表明,1961-2022年长江流域夏季热干旱事件的严重程度显著增加。其中,2013年和2022年是高温和高温和缺降水为主的两种不同类型的热干旱事件。在这两年,南亚高压东扩和西太平洋副热带高压西扩在印度洋高压上空建立了持续高压系统。2013年,西北印度洋较冷的海温异常促进了西风带异常,减少了西南向该地区的水汽输送。同时,位于东海上空的西北太平洋反气旋(WNPAC)促进了来自太平洋的有限水汽流入。这种结构主要由持续的高压系统控制,导致高温主导的复合事件。相比之下,2022年的奥运会表现出更大的复杂性。孟加拉湾温暖的海温异常增强了对流活动,增强了当地Hadley环流,促进了YRV上空的下降运动。受松山-吉尔响应的影响,西风增强,使西北太平洋向西延伸,热带水汽输送发生改变,导致对流层明显下降,热带气旋上空水汽不足。负的对流层位涡异常通过陆-气相互作用进一步加剧了复合事件,包括降水稀少、土壤干燥和地表感热通量增加。因此,2022年的事件比2013年的事件更加严重和多方面。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Elucidating the Varied Characteristics of Compound Hot–Drought From Two Distinctive Extreme Events in the Yangtze River Valley

Compound hot-drought events exert profound impacts on ecosystems, agriculture and public health, highlighting the need to understand their characteristics and driving mechanisms for effective climate change mitigation and adaptation strategies. This study reveals that the severity of summer hot–drought events in the Yangtze River Valley (YRV) significantly increased during 1961–2022. Among these, 2013 and 2022 represent two distinct types of hot-drought events: High-temperature and both high-temperature and deficient precipitation dominated. In both years, the eastward expansion of the South Asian High and the westward extension of the Western Pacific Subtropical High established persistent high-pressure systems over the YRV. In 2013, cooler sea surface temperature (SST) anomalies in the Northwestern Indian Ocean promoted the anomalous westerly, reducing the southwest water vapour transport to the region. Concurrently, the Western North Pacific anticyclone (WNPAC) positioned over the East China Sea facilitated limited moisture inflow from the Pacific. This configuration, mainly governed by persistent high-pressure systems, resulted in high-temperature-dominated compound events. In contrast, the 2022 event displayed greater complexity. Warmer SST anomalies in the Bay of Bengal intensified convective activity, enhancing the local Hadley circulation and promoting descending motion over the YRV. Strengthened easterly, influenced by the Matsuno–Gill response, contributed to the westward extension of the WNPAC and altered tropical water vapour transport, causing pronounced tropospheric descent and moisture deficits over the YRV. Negative tropospheric potential vorticity anomalies further exacerbated the compound event through land-atmosphere interactions, including scarce precipitation, soil drying and increased surface sensible heat flux. Consequently, the 2022 event was more severe and multifaceted than that in 2013.

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来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
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