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Simulation of the evolution of the latent heat processes in a mesoscale convective system accompanied by heavy rainfall over the Guangzhou region of South China

Simulation of the evolution of the latent heat processes in a mesoscale convective system accompanied by heavy rainfall over the Guangzhou region of South China

作     者:LI Jiang-Nan WU Kai-Lu DING Cheng-Hui YANG Chao-Feng LI Fang-Zhou WANG Dong-Hai FENG Ye-Rong LI Jiang-Nan;WU Kai-Lu;DING Cheng-Hui;YANG Chao-Feng;LI Fang-Zhou;WANG Dong-Hai;FENG Ye-Rong

作者机构:School of Atmospheric SciencesSun Yat-sen UniversityGuangzhouChina State Key Laboratory of Severe Weather(LaSW)Chinese Academy of Meteorological SciencesBeijingChina Guangdong/CMA Key Laboratory of Regional Numerical Weather PredictionGuangzhouChina 

出 版 物:《Atmospheric and Oceanic Science Letters》 (大气和海洋科学快报(英文版))

年 卷 期:2017年第10卷第1期

页      面:58-64页

核心收录:

学科分类:07[理学] 070601[理学-气象学] 0706[理学-大气科学] 

基  金:funded by the National Natural Science Foundation of China[grant number 41275060] the State Key Laboratory of Severe Weather Foundation of Chinese Academy of Meteorological Sciences The National Key Research and Development Program of China[grant number 2016YFA0602701] 

主  题:Mesoscale convective system microphysical process latent heat budget 

摘      要:A cloud-scale WRF simulation was used to investigate the cloud microphysical processes and threedimensional structure of latent heat budgets in different stages of a mesoscale convective system(MCS) accompanied by heavy rain that occurred in the Guangzhou region of South *** results enable us to draw the following conclusions:(1) During the development and mature stages,the main heating processes were condensation below 400 hPa and deposition above 400 *** main cooling processes were evaporation and *** the dissipation stage,all the microphysical processes were weak.(2) Water vapor condensed into cloud water,and rainwater significantly contributed to all stages of the MCS.(3) During every stage of the MCS,the primary cooling microphysical process was the evaporation of rainwater,which was maximum during the mature stage.

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