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EFFECTS OF THREE-DIMENSIONAL STRUCTURE OF HEATING FIELD ON THE SUMMER MONSOON CIRCULATION IN ASIA
引用本文:Lin Ben,Zhang Jinsong. EFFECTS OF THREE-DIMENSIONAL STRUCTURE OF HEATING FIELD ON THE SUMMER MONSOON CIRCULATION IN ASIA[J]. , 1990, 4(3): 343-353
作者姓名:Lin Ben  Zhang Jinsong
作者单位:Department of Geophysics Peking University,Beijing,Department of Geophysics,Peking University,Beijing
摘    要:In this paper,a primitive equation linear wave model is used to examine the effects of three-dimen-sional structure of heating field on the behavior of stationary planetary waves in summer and to comparethe roles of different heating functions for the formation and maintenance of summer monsoon circulationin Asia.It is shown that the aloft heating connected with the latent heating,especially the deep condensationheating associated with the cumulus convection in low latitudes,plays a crucial part in the Asian summer mon-soon and the structures of planetary wave responses are quite sensitive to the vertical distribution of heating.

收稿时间:1989-09-18

EFFECTS OF THREE-DIMENSIONAL STRUCTURE OF HEATING FIELD ON THE SUMMER MONSOON CIRCULATION IN ASIA
Lin Benda and Zhang Jinsong. EFFECTS OF THREE-DIMENSIONAL STRUCTURE OF HEATING FIELD ON THE SUMMER MONSOON CIRCULATION IN ASIA[J]. Acta Meteorologica Sinica, 1990, 4(3): 343-353
Authors:Lin Benda and Zhang Jinsong
Affiliation:Department of Geophysics, Peking University, Beijing;Department of Geophysics, Peking University, Beijing
Abstract:In this paper,a primitive equation linear wave model is used to examine the effects of three-dimensional structure of heating field on the behavior of stationary planetary waves in summer and to compare the roles of different heating functions for the formation and maintenance of summer monsoon circulation in Asia.It is shown that the aloft heating connected with the latent heating,especially the deep condensation heating associated with the cumulus convection in low latitudes,plays a crucial part in the Asian summer monsoon and the structures of planetary wave responses are quite sensitive to the vertical distribution of heating.
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