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西南地区特大干旱大气环流特征分析

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采用区域降水指数选取1992、2006和2009年为西南地区特大干旱年,并利用1961-2010年143个测站的逐日降水资料以及NCEP/NCAR再分析资料分析了3年的降水时间分布特征及500hPa高度场和整层水汽输送的异常特征.结果表明:3个特大干旱年的少雨时段均集中在6-9月.高度场及其信号场具有一定的空间特征,西南地区被高压系统控制,位势高度偏高,且在异常气旋式水汽通道的东北异常水汽控制之下,减弱了来自孟加拉湾和南海的水汽输送,是导致西南地区持续干旱的重要原因.
Research on the Anomalies of Atmospheric Circulation of the Extremely Severe Drought in Southwest China
The 1992 drought,the 2006 drought and the 2009-2010 drought were identified as the extremely severe drought according to the precipitation index.Based on the NCEP/NCAR reanalysis data and the daily precipitation data of the 143 stations in Southwest China from 1961 to 2010,the temporal distributive features of the extremely severe drought and the anomalous atmospheric circulation in drought period are analyzed.Results show that the rainless period starts from June and ends in September.In the drought period,the evolution of height field and normalized field has regional characteristics:southwest China is controlled by high pressure system with higher geo-potential height.Moreover,the water vapor transport from the bay of Bengal and South China Sea was reduced under the control of abnormal northeast moisture,which resulted in the persistence of the extraordinary drought.

Southwest Chinadroughtprecipitationheight fieldwater vapor field

费玲玲、陆桂华、吴志勇、何海、何健

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河海大学水文水资源学院,南京210098

河海大学水问题研究所,南京210098

西南地区 干旱 降水 高度场 水汽输送

水利部公益性行业科研专项经费项目全国优秀博士学位论文作者专项资金资助项目教育部新世纪优秀人才支持计划

201301040201161NCET-12-0842

2014

中国农村水利水电
水利部中国灌溉排水发展中心 水利部农村水电及电气化发展局 武汉大学 中国国家灌溉排水委员会

中国农村水利水电

CSTPCD北大核心
影响因子:0.655
ISSN:1007-2284
年,卷(期):2014.(8)
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