长江流域地区水汽输送及其对旱涝影响研究综述  

The review of water vapor transportation and its effects on drought and flood over China

作　　者：蒋兴文[1] 李跃清[1] 

机构地区：[1]中国气象局成都高原气象研究所,成都610071

出　　处：《气象科学》2009年第1期138-142,共5页Journal of the Meteorological Sciences

基　　金：干旱气象科学研究基金项目(IAM200710);江苏省气象灾害重点实验室项目(KLME050210)

摘　　要：大气水汽输送在气候系统中起着重要的作用。本文回顾了近年来关于长江流域地区水汽输送的相关研究进展,主要包括长江流域水汽输送的基本特征,旱涝年水汽输送的异常特征,青藏高原对长江流域水汽输送的影响,青藏高原水汽输送与长江流域旱涝的关系。The water vapor transport plays an important role in the climate system. The research on water vapor transportation over Ya.gtze River in recent years has been reviewed in this paper. It mainly ineludes the basic status of water vapor transportation over Yangtze River ,the anomaly status of water vapor transportation in dry or flood years, the effects of Tibetan Plateau on water vapor transportation over Yangtze River, the correlation between water vapor transport over Tibetan Plateau and drought or flood in Yangtze River.

关 键 词：水汽输送 长江流域旱涝 综述 

分 类 号：P434.5[天文地球—大气科学及气象学]