The Theory Study of the Influence of the Topography on the Cold Frontal Motion

Gu Wei; Wu Rongsheng

doi:10.1007/BF02657507

Impact Factor: 5.8

Volume 9 Issue 2

Mar. 1992

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1992 > 9(2): 167-172

The Theory Study of the Influence of the Topography on the Cold Frontal Motion

1.
Department of Atmospheric Sciences, Nanjing University, Nanjing 210008,Department of Atmospheric Sciences, Nanjing University, Nanjing 210008

doi: 10.1007/BF02657507

Abstract
References
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Abstract:
In order to study the characteristics of cold frontal motion over the arbitrary topography, the velocity of cold frontal movement is derived by using the one layer shallow-water model. The results show that there exist the retardation in upwind side and rapid descent in the lee slope when the cold front crosses the topography.
References

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Manuscript History

Manuscript received: 10 March 1992

Manuscript revised: 10 March 1992

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

The Theory Study of the Influence of the Topography on the Cold Frontal Motion

1. Department of Atmospheric Sciences, Nanjing University, Nanjing 210008,Department of Atmospheric Sciences, Nanjing University, Nanjing 210008

Manuscript received: 1992-03-10
Manuscript revised: 1992-03-10

Abstract: In order to study the characteristics of cold frontal motion over the arbitrary topography, the velocity of cold frontal movement is derived by using the one layer shallow-water model. The results show that there exist the retardation in upwind side and rapid descent in the lee slope when the cold front crosses the topography.