首页> 中文期刊> 《气象学报:英文版》 >Organized Warm-Sector Rainfall in the Coastal Region of South China in an Anticyclone Synoptic Situation:Observational Analysis

Organized Warm-Sector Rainfall in the Coastal Region of South China in an Anticyclone Synoptic Situation:Observational Analysis

         

摘要

Organized warm-sector rainfall(OWSR)near the coast of South China tends to occur in certain synoptic situations characterized with either a low-level jet or an anticyclone,with the latter being less investigated.This paper fills the gap by analyzing 15 OWSR events that occurred in an anticyclone synoptic situation during the pre-summer rainy season of 2011-2016,based on high-resolution observational and reanalysis data.The results show that the anticyclone synoptic situation produces marked northerly boundary-layer winds inland and obvious northeasterly,easterly/southwesterly,and southeasterly boundary-layer winds near the coasts of eastern Guangdong,western Guangdong,and Guangxi,respectively.The coastal boundary-layer winds promote favorable environmental conditions and strong convergence for convection initiation;consequently,OWSR is prone to occur near the coasts of western Guangdong and Guangxi,but exhibits different formation and propagation features in the following two subareas.(1)The southeasterly boundary-layer winds tend to converge near the border area between Guangxi and Guangdong(BGG),promoting the formation of a stable convective line along the mountains.The convective line persists with support of upper-level southwesterly winds that facilitate convective cells to propagate along the convective line,producing heavy OWSR along the mountains near BGG.(2)In contrast,a west-east convective line tends to form and maintain near the coast of Yangjiang(YJ)area,about 200 km east of BGG,owing to stable convergence between the easterly(or southwesterly)and the northerly boundary-layer winds reinforced by the mountains near YJ.Moreover,the coupling of upper-level westerly winds with the easterly(southwesterly)boundary-layer winds facilitates expansion(eastward propagation)of the convective line,causing west-east-oriented heavy OWSR near the coast of YJ.In a word,this study reveals refined properties of OWSR initiation and development in the anticyclone synoptic situation,which may help improve the forecast skill of OWSR during the pre-summer rainy season in South China.

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