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Volume 7 Issue 2

Mar.  1990

Article Contents

Analysis and Study of a Mesoscale Inertia-Gravitational Wave in Upper Air


doi: 10.1007/BF02919160

  • A mesoscale inertia-gravitational wave at 200 hPa is analysed. The reasons of this wave occurring are also dis-cussed. It is indicated that the occurrence of this wave is due to inertia-gravitational instability, and closely related to horizontal and vertical shear of wind.
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Manuscript History

Manuscript received: 10 March 1990
Manuscript revised: 10 March 1990
通讯作者: 陈斌, bchen63@163.com
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Analysis and Study of a Mesoscale Inertia-Gravitational Wave in Upper Air

  • 1. Laboratory for Numerical Modeling of Atmospheric Sciences and Geophysical Fluid Dynamics, Academia Sinica, Beijing, 100080,Laboratory for Numerical Modeling of Atmospheric Sciences and Geophysical Fluid Dynamics, Academia Sinica, Beijing, 100080,Laboratory for Numerical Modeling of Atmospheric Sciences and Geophysical Fluid Dynamics, Academia Sinica, Beijing, 100080

Abstract: A mesoscale inertia-gravitational wave at 200 hPa is analysed. The reasons of this wave occurring are also dis-cussed. It is indicated that the occurrence of this wave is due to inertia-gravitational instability, and closely related to horizontal and vertical shear of wind.

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