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地理科学 >

1994 , Vol. 14 >Issue 4: 347 - 354,391

DOI: https://doi.org/10.13249/j.cnki.sgs.1994.04.347

论文

东北地形对强对流天气影响的分析

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  • 吉林省气象台 长春130062

收稿日期: 1992-09-01

  网络出版日期: 1994-07-20

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THE ANALYSIS OF THE EFFECTS OF TOPOGRAPHY IN NORTHEAST CHINA ON STRONG COVECTION WEATHER

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  • Meteorological Observatory of Jilin Province, Changchun 130062

Received date: 1992-09-01

  Online published: 1994-07-20

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摘要

通过对发生在吉林省境内的强对流天气分布及造成强对流天气的中尺度系统与东北地形关系的分析,指出东北地形对强对流天气的影响,以及强对流天气在天气预报中的作用.

本文引用格式

王晓明, 谢静芳 . 东北地形对强对流天气影响的分析[J]. 地理科学, 1994 , 14(4) : 347 -354,391 . DOI: 10.13249/j.cnki.sgs.1994.04.347

Abstract

In this paper, the ralation of the distribution of strong convection weather occurring in Jilin Province and the mesoscale weather system causing strong convection weather to the topography in Northeast China was analysed. The analysis results can be used as a reference for forecasting the strong convection weather.

参考文献

1. 李麦村.重力波对特大暴雨的触发作用.大气科学,1978.2(3):201~109.
2. 斯公望.暴雨和强对流环流系统.北京:气象出版社.330~336.
3. 杨国样,何齐强,张汉城.中尺度气象学.北京:气象出版社.1991. 144~154.
4. 刘金玉,张义增.根据地面要素场制作强对流天气的短时预报.气象,1985.11(11):5~10.
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