THE NUMERICAL EXPERIMENTS ON DYNAMIC FORCING BY THE TIBETAN PLATEAU FOR VARIOUS ZONAL FLOWS

Chen Yuxiang; Ji Liren; Shen Rujin

doi:10.1007/BF03179751

Impact Factor: 5.8

Volume 2 Issue 2

Apr. 1985

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1985 > 2(2): 189-199

THE NUMERICAL EXPERIMENTS ON DYNAMIC FORCING BY THE TIBETAN PLATEAU FOR VARIOUS ZONAL FLOWS

1.
Institute of Atmospheric Physics, Academia Sinica, Beijing,Institute of Atmospheric Physics, Academia Sinica, Beijing,Institute of Atmospheric Physics, Academia Sinica, Beijing

doi: 10.1007/BF03179751

Abstract
References
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Abstract:
In this paper, the dynamic disturbances to various basic zonal currents caused by the Tibetan Plateau are simulated by means of a three-level primitive equation model, in which σ is used as the vertical coor-dinate. Four types of currents have been used, i. e. the barotropic homogeneous current, barotropic jet stream, baroclinic current and the zonal mean current in summer. The results are helpful to understand the dynamic effects of the Tibetan Plateau on the general circulation over East Asia.
References

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Manuscript History

Manuscript received: 10 April 1985

Manuscript revised: 10 April 1985

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 NUMERICAL EXPERIMENTS ON DYNAMIC FORCING BY THE TIBETAN PLATEAU FOR VARIOUS ZONAL FLOWS

1. Institute of Atmospheric Physics, Academia Sinica, Beijing,Institute of Atmospheric Physics, Academia Sinica, Beijing,Institute of Atmospheric Physics, Academia Sinica, Beijing

Manuscript received: 1985-04-10
Manuscript revised: 1985-04-10

Abstract: In this paper, the dynamic disturbances to various basic zonal currents caused by the Tibetan Plateau are simulated by means of a three-level primitive equation model, in which σ is used as the vertical coor-dinate. Four types of currents have been used, i. e. the barotropic homogeneous current, barotropic jet stream, baroclinic current and the zonal mean current in summer. The results are helpful to understand the dynamic effects of the Tibetan Plateau on the general circulation over East Asia.