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Dynamic Features and Maintenance Mechanism of Asian Summer Monsoon Subsystem


doi: 10.1007/s00376-999-0028-x

  • In the context of the dissociation of vertical shear flow and tropospheric mean flow based on 1980-1996 NCEP / NCAR re-analysis, study is undertaken of the barotropic and baroclinic de-velopment characteristics and kinetic energy maintenance mechanisms of Asian summer monsoon. Evidence suggests that the monsoon activity is marked by noticeable baroclinicity in three active regions of different dynamical characteristics, located in India, East Asian tropics and subtropics, respectively, with greatly differing maintenance mechanisms of barotropic / baroclinic kinetic en-ergy.
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Manuscript History

Manuscript received: 10 October 1999
Manuscript revised: 10 October 1999
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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Dynamic Features and Maintenance Mechanism of Asian Summer Monsoon Subsystem

  • 1. State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASC), Institute of Atmospheric Physics. Chinese Academy of Sciences, Beijing 100080,State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASC), Institute of Atmospheric Physics. Chinese Academy of Sciences, Beijing 100080

Abstract: In the context of the dissociation of vertical shear flow and tropospheric mean flow based on 1980-1996 NCEP / NCAR re-analysis, study is undertaken of the barotropic and baroclinic de-velopment characteristics and kinetic energy maintenance mechanisms of Asian summer monsoon. Evidence suggests that the monsoon activity is marked by noticeable baroclinicity in three active regions of different dynamical characteristics, located in India, East Asian tropics and subtropics, respectively, with greatly differing maintenance mechanisms of barotropic / baroclinic kinetic en-ergy.

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