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作 者:CAO Jie XU Qin GAO Shou-Ting
机构地区:[1]Institute of Atmospheric Physics, Chinese Academy of Sciences [2]Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma [3]National Severe Storms Laboratory
出 处:《Atmospheric and Oceanic Science Letters》2015年第6期403-408,共6页大气和海洋科学快报(英文版)
基 金:supported by the National Basic Research Program of China(Grant No.2012CB417201);the National Science and Technology Support Program(Grant No.GYHY201406001);the National Natural Science Foundation of China(Grant No.41205033);the Key Project of the Key Laboratory of Atmosphere and Environments on the Plateau in Sichuan Province(Grant No.PAEKL-2014-C1)
摘 要:After first reviewing historical and current difficulties in solving streamfunction and velocity potential in a limited domain,and describing recent developments in obtaining accurate solutions in a limited domain with arbitrary shape,a newly proposed approach is introduced and its application to a torrential rain event is reported.The results show that the newly developed method has advantages in capturing mesoscale information,compared with horizontal winds.After first reviewing historical and current difficulties in solving streamfunction and velocity potential in a limited domain,and describing recent developments in obtaining accurate solutions in a limited domain with arbitrary shape,a newly proposed approach is introduced and its application to a torrential rain event is reported.The results show that the newly developed method has advantages in capturing mesoscale information,compared with horizontal winds.
关 键 词:streamfunction VELOCITY potential LIMITED DOMAIN m
分 类 号:P456.7[天文地球—大气科学及气象学]
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