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STUDY OF CHARACTERISTIC MODES IN SIMPLE TROPICAL COUPLED AIR-SEA MODEL
作者姓名:Zhang  Xiangdong
作者单位:Department of
摘    要:The propagation features, stabilities and dynamical characteristic structures of coupled Kelvin inner modes andsecond order Rossby inner modes are studied using a simple tropical coupled air-sea model in this paper. It is shownthat there is mechanism of selecting scale and frequency in the tropical air-sea system. The effects of air-sea couplingare mainly on the large-scale modes and nonuniform. These effects make the frequency of Kelvin modes decrease andeven excite the eastward propagating Rossby inner modes. These effects make the unstable development of Kelvinmodes and result in the decay of Rossby modes. The effects of atmospheric damp are opposite to those of air-sea coup-ling. The oceanic damp only make the wave amplitudes decay. Simutaneously, this paper shows the dynamical character-istic structures of air-sea coupled system and the phase relations between the atmospheric and the oceanic wave compo-nent.

收稿时间:6/3/1991 12:00:00 AM

STUDY OF CHARACTERISTIC MODES IN SIMPLE TROPICAL COUPLED AIR-SEA MODEL
Zhang Xiangdong.STUDY OF CHARACTERISTIC MODES IN SIMPLE TROPICAL COUPLED AIR-SEA MODEL[J].Acta Meteorologica Sinica,1992,6(3):287-298.
Authors:Zhang Xiangdong
Institution:Zhang Xiangdong Department of Atmospheric Sciences,Nanjing University,Nanjing 210008
Abstract:The propagation features, stabilities and dynamical characteristic structures of coupled Kelvin inner modes and second order Rossby inner modes are studied using a simple tropical coupled air-sea model in this paper. It is shown that there is mechanism of selecting scale and frequency in the tropical air-sea system. The effects of air-sea coupling are mainly on the large-scale modes and nonuniform. These effects make the frequency of Kelvin modes decrease and even excite the eastward propagating Rossby inner modes. These effects make the unstable development of Kelvin modes and result in the decay of Rossby modes. The effects of atmospheric damp are opposite to those of air-sea coup- ling. The oceanic damp only make the wave amplitudes decay. Simutaneously, this paper shows the dynamical character- istic structures of air-sea coupled system and the phase relations between the atmospheric and the oceanic wave compo- nent.
Keywords:air-sea coupling  Kelvin modes  Rossby modes
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