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投稿时间：2007-02-07 修订日期：2007-07-05
投稿时间：2007-02-07 修订日期：2007-07-05
中文摘要: 华北回流天气是预报中的难题，尤其是对其产生降水的开始和结束时间和华北回流的
性质研究不多。作者使用NCEP再分析资料、实时观测资料和中尺度模式MM5，对一次回流
暴雪过程进行了诊断分析和数值试验。通过分析和试验得出了一些有意义的结果:回流降水
的开始和结束与高低层的风向有关，中高层的西南气流与低层偏东气流叠加时降水开始，两
者之一消失降水结束；低层经渤海回流到华北地区的气团是干冷的；回流降水的水汽伴随中
层的西南气流来自南方地区。这在实际业务预报中具有很好的指示意义。
Abstract:It is difficult to forecast the return flow weather which occurred over North C
hina. In order to reveal the mechanism of return flow weather, such as the character o
f return flow, a heavy snow of return flow weather which occurred over North C
hina was diagnosed and investigated by using NCEP data and the Pennsylvania State Univers
ity NCAR Fifth Generation Mesoscale Model (MM5), version 3. The results show t
hat the start and end time of precipitation was closely related to the wind direct
ion, including the upper warm and humid air and lower cold air. The lower layer
air from Northeast Plain through Bohai Sea was drier and colder than the upper air f
rom southwest. The moisture of return flow weather mainly came from southwest w
ith southwestern flow.
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基金项目:中国气象局气象灾害天气国家重点实验室开放课题CMATG2005Y06资助
引用文本：
张迎新,侯瑞钦,张守保,2007.回流暴雪过程的诊断分析和数值试验[J].气象,33(9):25-32.
Zhang Yingxin,Hou Ruiqin,Zhang Shoubao,2007.Numerical Experiments and Diagnosis on a Heavy Snow of Return flow Events[J].Meteor Mon,33(9):25-32.
张迎新,侯瑞钦,张守保,2007.回流暴雪过程的诊断分析和数值试验[J].气象,33(9):25-32.
Zhang Yingxin,Hou Ruiqin,Zhang Shoubao,2007.Numerical Experiments and Diagnosis on a Heavy Snow of Return flow Events[J].Meteor Mon,33(9):25-32.