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我国西南地区夏季长周期旱涝急转及其大气环流异常

孙小婷 李清泉 王黎娟

大气科学2017,Vol.41Issue(6):1332-1342,11.
大气科学2017,Vol.41Issue(6):1332-1342,11.DOI:10.3878/j.issn.1006-9895.1705.16282

我国西南地区夏季长周期旱涝急转及其大气环流异常

Characteristics of Long-Cycle Abrupt Drought-Flood Alternations in Southwest China and Anomalies of Atmospheric Circulation in Summer

孙小婷 1李清泉 2王黎娟1

作者信息

  • 1. 南京信息工程大学气象灾害教育部重点实验室/气候与环境变化国际合作联合实验室/气象灾害预报预警与评估协同创新中心,南京210044
  • 2. 国家气候中心中国气象局气候研究开放实验室,北京100081
  • 折叠

摘要

Abstract

Based on daily precipitation data collected at 567 stations in China from 1961 to 2015,an index of abrupt drought-flood alternation in Southwest China in summer was defined.The results show that the alternation events from drought to flood are more than those from flood to drought in the summers during 1961-1970,the alternations from flood to drought are more during 1971-1980,and the alternations from drought to flood are equal to those from flood to drought during 1981-2000.Since the early 21st century,abrupt alternations from flood to drought tend to increase.Typical abrupt drought-flood alternation events in summer were selected and the characteristics of the anomalous atmospheric circulation and water vapor transportation were analyzed.It was found that the western Pacific subtropical high extended westward and became stronger during the drought period before the conversion from drought to flood.The westerlies at the middle and high latitudes also became stronger,preventing cold air from moving southward.In the vertical,downdrafi prevailed and the moisture transport from the Bay of Bengal and South China Sea was weaker than before.Southwest China was located at the moisture divergence area.In addition,there was less rainfall during drought periods.During the flood period after the conversion from drought to flood,meridional circulation at the middle and high latitudes tended to be stronger.The trough to the east of the Ural Mountains deepened and the eastern Asia ridge strengthened.The westerlies at the middle and high latitudes became weaker and updrafts prevailed in the vertical.Also,large amounts of moisture were transported from the Bay of Bengal and South China Sea to Southwest China,which explains why rainfall became abundant there.The opposite was true in the years of conversion from flood to drought.

关键词

西南地区/旱涝急转/大气环流/水汽输送

Key words

Southwest China/Drought-flood abrupt alternation/Atmospheric circulation/Moisture transportation

分类

天文与地球科学

引用本文复制引用

孙小婷,李清泉,王黎娟..我国西南地区夏季长周期旱涝急转及其大气环流异常[J].大气科学,2017,41(6):1332-1342,11.

基金项目

国家重点基础研究发展计划项目2013CB430202、 2012CB955203 National Basic Research Program of China (Grants 2013CB430202 and 2012CB955203) (Grants 2013CB430202 and 2012CB955203)

大气科学

OA北大核心CSCDCSTPCD

1006-9895

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