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2022年长江流域极端高温干旱的环流异常特征及其影响机制

孙昭萱 张强 周长艳 廖倬纤

气象学报2026,Vol.84Issue(3):486-499,14.
气象学报2026,Vol.84Issue(3):486-499,14.DOI:10.11676/qxxb2026.20250105

2022年长江流域极端高温干旱的环流异常特征及其影响机制

Atmospheric circulation anomalies and impact mechanisms behind the extreme heat and drought event over the Yangtze River Basin in 2022

孙昭萱 1张强 2周长艳 1廖倬纤3

作者信息

  • 1. 四川省气候中心,高原与盆地暴雨旱涝灾害四川省重点实验室,成都,610072
  • 2. 甘肃省气象局,兰州,730020||中国气象局兰州干旱气象研究所,甘肃省干旱气候变化与减灾重点实验室,中国气象局干旱气候变化与减灾重点开放实验室,兰州,730020
  • 3. 瓦赫宁根大学与研究中心,瓦赫宁根,6700 HB
  • 折叠

摘要

Abstract

In the midsummer of 2022,the Yangtze River Basin experienced a historically rare extreme compound event of high temperature and drought.Investigating its causes and impact mechanisms is of great significance for the scientific understanding of extreme climate events.This study utilizes daily maximum temperature observations collected at 720 national meteorological stations across the Yangtze River Basin and the meteorological drought composite index(MCI)as well as the NCEP/NCAR reanalysis data to systematically analyze atmospheric circulation anomalies and influencing mechanisms of sea surface temperature(SST)as an external forcing.Results indicate that during the summer of 2022,the Western Pacific subtropical high(WPSH)and South Asian high(SAH)exhibited unprecedented intensification and dominated the Yangtze River Basin,with their intensities reaching historical extremes.An abnormally northward shifted 200 hPa subtropical westerly jet(SWJ)formed a warm ridge,effectively blocking the convergence of cold and warm air masses.The Yangtze River Basin was controlled by an anomalous anticyclonic circulation,which led to significant water vapor divergence.The re-intensification of the La Niña event and the record-breaking strengthening of the negative phase of the tropical Indian Ocean dipole(TIOD)jointly enhanced the descending branches of both the Walker and Hadley circulations,which,aided by the SWJ,further intensified the deep high-pressure system over the Yangtze River Basin,ultimately resulting in the prolonged extreme high temperature and drought event.It is worth noting that the interdecadal warming of the Indian Ocean warm pool(IOWP)and the Western Pacific warm pool(WPWP)has led to increasingly significant impacts on the WPSH and SAH.Their influences have exceeded that of SST anomalies in the equatorial central-eastern Pacific,making them key predictors for sub-seasonal to seasonal forecasting.

关键词

极端高温干旱复合事件/大气环流异常/拉尼娜/暖池海温/长江流域

Key words

Extreme heat and drought event/Anomalies of atmospheric circulation/La Niña/Warm pool sea surface temperature/Yangtze River Basin

分类

天文与地球科学

引用本文复制引用

孙昭萱,张强,周长艳,廖倬纤..2022年长江流域极端高温干旱的环流异常特征及其影响机制[J].气象学报,2026,84(3):486-499,14.

基金项目

国家自然科学基金重点项目(42230611)、四川省自然科学基金项目(2024NSFSC0066). (42230611)

气象学报

0577-6619

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