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《Chinese Journal of Atmospheric Sciences》 2007-06
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A Quantitative Diagnosis for the Mechanisms of Spring Droughts in South China

WEN Zhi-Ping1,WU Nai-Geng1,2,FENG Ye-Rong1,2,LIN Liang-Xun2,YUAN Zhuo-Jian1,and CHEN Bing-Hong1,21 Center for Monsoon and Environment Research/Department of Atmospheric Sciences,Sun Yat-Sen University,Guangzhou 5102752 Guangzhou Meteorological Observatory,Guangzhou 510080  
Since spring droughts in South China(SC) are mainly characterized by the absence of uplifting of moist southerly,it is necessary to carry out an overall quantitative investigation for the forced-local-meridional circulation over SC.With a complete(including dynamic and thermodynamic mechanisms) linear-diagnostic model for the local-meridional circulation and the NCEP/NCAR reanalysis data, the present numerical study show that the contributions to the lower layer subsidence in SC are mainly from the forcing processes associated with the latent heat in the baroclinic troughs located to the north of SC(the compensatory subsidence accounting for 56% of the lower-layer divergence in SC),meridional temperature advection(25%) and the zonal advection of zonal momentum(20%).All of them point to the abnormal northward shift of the baroclinic troughs embedded in the general circulation characterized by the presence of blocking highs around the Ural Mountains and the sinificant northwestward extension of the western Pacific subtropical high(WPSH) for the composite spring droughts in SC.For an extrem dry case(i.e.the 1991 spring drought in SC),the variation of the Ural high was 2-6 days prior to that of the WPSH.
【Fund】: 国家自然科学基金重点项目40730951;; 国家重点基础研究发展规划项目2004CB418303;; 国家自然科学基金资助项目40575021;; 广东省科技计划重点引导项目2005B32601008
【CateGory Index】: P462.3
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