Numerical Experiments of Meiyu(Baiu) Rainfall by Quasi-Lagrangian Limited Area Model with Terrain

Zhao Li; Zhao Sixiong

doi:10.1007/BF02661287

Impact Factor: 5.8

Volume 12 Issue 1

Jan. 1995

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1995 > 12(1): 57-66

Numerical Experiments of Meiyu(Baiu) Rainfall by Quasi-Lagrangian Limited Area Model with Terrain

1.
InstituteofAtmosphericPhysics,ChineseAcademyofSciences,Beijing100080,InstituteofAtmosphericPhysics,ChineseAcademyofSciences,Beijing100080

doi: 10.1007/BF02661287

Abstract
References
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Abstract:
In this paper, a 10-level Quasi-Lagrangian Limited Area Model is used to simulate the process of Meiyu(Baiu) front of 1979. Some physical processes, such as large-scale condensation and cumulus convection, are included in the model. The simulation results are encouraging. 24-h numerical simulation shows that the invading of cold air from North China and rapidly northward moving of warm air from South China can be successfully reproduced. The terrain with a maximum of 4175 m is incorporated in the model. Three different kinds of terrain schemes are tested and the dynamic effect of the Plateau on the process of heavy rainfall is found to be very important.
- Meiyu,
- Rainband,
- Quasi-lagrangian,
- Model
References

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Manuscript History

Manuscript received: 10 January 1995

Manuscript revised: 10 January 1995

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

Numerical Experiments of Meiyu(Baiu) Rainfall by Quasi-Lagrangian Limited Area Model with Terrain

1. InstituteofAtmosphericPhysics,ChineseAcademyofSciences,Beijing100080,InstituteofAtmosphericPhysics,ChineseAcademyofSciences,Beijing100080

Manuscript received: 1995-01-10
Manuscript revised: 1995-01-10

Abstract: In this paper, a 10-level Quasi-Lagrangian Limited Area Model is used to simulate the process of Meiyu(Baiu) front of 1979. Some physical processes, such as large-scale condensation and cumulus convection, are included in the model. The simulation results are encouraging. 24-h numerical simulation shows that the invading of cold air from North China and rapidly northward moving of warm air from South China can be successfully reproduced. The terrain with a maximum of 4175 m is incorporated in the model. Three different kinds of terrain schemes are tested and the dynamic effect of the Plateau on the process of heavy rainfall is found to be very important.

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