IMPACT OF SSTA OF SOUTHERN HEMISPHERE ON FLOOD SEASON PRECIPITATION ANOMALIES IN YUNNAN  

作　　者：杨竹云 杨素雨 严华生 张瑾文 古书鸿 

机构地区：[1]Meteorological Observatory of Yunnan [2]Department of Atmospheric Science,Yunnan University [3]Guizhou Institute of Mountainous Environment and Climate

出　　处：《Journal of Tropical Meteorology》2015年第3期255-264,共10页热带气象学报（英文版）

基　　金：National Natural Science Foundation of China(41075072,41065004);National Natural Science Foundation of China-Yunnan Province Joint Foundation(U0833602);Specialized Project for Forecasters in Yunnan Province(YB201202);Project for Fourth Program of Undergraduates in Yunnan Province(ynuy201154);Integration and Demonstration of Techniques for Mitigating and Controlling Eruptive Disasters in Southwest China,a project of National Science and Technology Support for the 12th Five-Year Economic Development(2012BAD20B06)

摘　　要：Based on the reanalysis data of monthly mean global SST and wind from the NCEP/NCAR and the observation data of rain seasons in 124 stations of Yunnan province from 1961 to 2006, we applied the analytical methods of correlation analysis and composite analysis and a significance testing method to two sets of samples of average differences. The goal is to investigate into the influence of the Southern Hemispheric(SH) SST on the summer precipitation in Yunnan from January to May so as to identify the key time and marine regions. Physical mechanisms are obtained by analyzing the influence of sea level wind and the key marine regions on the precipitation during Yunnan's rain season.Results show that there is indeed significant relationship between the SST in SH and summer precipitation in Yunnan.The key areas for influencing the summer precipitation are mainly distributed in a region called "West Wind Drift" in the SH, including the Southeast Indian, southern Australia, west coast of eastern Pacific off Chile, Peru and the southwest Atlantic Magellan. Besides, the most significant marine region is the west coast of Chile and Peru(cold-current areas of the eastern Pacific). Diagnostic analysis results also showed that monsoons in the Bay of Bengal, a cross-equatorial flow in the Indian Ocean near the equator and southwest monsoon in India weaken during the warm phase of the Peruvian cold current in the eastern Pacific. Otherwise, they strengthen.Based on the reanalysis data of monthly mean global SST and wind from the NCEP/NCAR and the observation data of rain seasons in 124 stations of Yunnan province from 1961 to 2006, we applied the analytical methods of correlation analysis and composite analysis and a significance testing method to two sets of samples of average differences. The goal is to investigate into the influence of the Southern Hemispheric（SH） SST on the summer precipitation in Yunnan from January to May so as to identify the key time and marine regions. Physical mechanisms are obtained by analyzing the influence of sea level wind and the key marine regions on the precipitation during Yunnan＇s rain season.Results show that there is indeed significant relationship between the SST in SH and summer precipitation in Yunnan.The key areas for influencing the summer precipitation are mainly distributed in a region called ＂West Wind Drift＂ in the SH, including the Southeast Indian, southern Australia, west coast of eastern Pacific off Chile, Peru and the southwest Atlantic Magellan. Besides, the most significant marine region is the west coast of Chile and Peru（cold-current areas of the eastern Pacific）. Diagnostic analysis results also showed that monsoons in the Bay of Bengal, a cross-equatorial flow in the Indian Ocean near the equator and southwest monsoon in India weaken during the warm phase of the Peruvian cold current in the eastern Pacific. Otherwise, they strengthen.

关 键 词：SST of Southern Hemisphere YUNNAN precipitation anomalies during rain season key marine area West Wind Drift 

分 类 号：P462.2[天文地球—大气科学及气象学]