本文已被:浏览 549次 下载 1224次
中文摘要: 根据各收支方程讨论,概述了各研究者采用直接和间接的方法,计算得出长江流域梅雨期暴雨过程中各种源汇的空间分布特征。虽然个例、地区和资料不同,其结果各有差异,也不易比较,但次网格尺度运动对大尺度环境场的反馈作用均非常显著,因而在设计暴雨预报的数值模式时,参数化方案是必不可少的。
中文关键词: 收支方程,参数化方案,梅雨期暴雨,积云对流,反馈作用
Abstract:On the basis of discussion about various budget equations,the horizontal pattern and vertical profiles of apparent source and sink with direct and indirect methods over the Changjiang River basin during Mei-yu heavy rain are summarized. Although the results are different and difficult to compare for each case,region or data,but this is certainly followed by an important vertical transport process of subgrid-scale,which reflects the striking effect of cumulus convection on largescale environment.Thus,for any prognostic models of heavy rain over the midlatitutes,it is necesary to add the parameterization of subgrid-scale motion.
keywords: calculation of budget,parameterization scheme,Meiyu beavy rain,cumulus convection feedback effect
文章编号: 中图分类号: 文献标志码:
基金项目:
Author Name | Affiliation |
引用文本:
汪钟兴,1994.暴雨过程中积云对流反馈作用的诊断研究[J].气象,20(2):3-10.
,1994.Diagnostic Studies of the Effect of Cumulus Convection on Large-Scale Environment[J].Meteor Mon,20(2):3-10.
汪钟兴,1994.暴雨过程中积云对流反馈作用的诊断研究[J].气象,20(2):3-10.
,1994.Diagnostic Studies of the Effect of Cumulus Convection on Large-Scale Environment[J].Meteor Mon,20(2):3-10.