| NUMERICAL EXPERIMENTS ON THE TROPICAL AIR-SEA INTERACTION WAVES |
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| 引用本文： | Zhang Renhe,Chao Jiping. NUMERICAL EXPERIMENTS ON THE TROPICAL AIR-SEA INTERACTION WAVES[J]. , 1992, 6(2): 148-158 |
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| 作者姓名： | Zhang Renhe Chao Jiping |
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| 作者单位： | Institute of Atmospheric Physics Academia Sinica，Beijing 100080，National Research Center for Marine Environmental Forecasts，State Oceanic Administration，Beijing 100081 |
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| 摘 要： | By means of the numerical method,the tropical air-sea interaction waves are studied.The results show that whenthe Kelvin waves are filtered out and only the equatorial Rossby waves are reserved both in the atmosphere and in theocean,the disturbances can also propagate eastward because of the air-sea interaction.The critical wavelength of theeastward propagating waves is related to the intensity of the air-sea interaction.The stronger the air-sea interaction,thelarger the eastward propagating components of the air-sea interaction waves.The results of the numerical experimentsare in good agreement with those of the theoretical analysis(Chao and Zhang,1988).
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| 收稿时间： | 1991-08-01 |
NUMERICAL EXPERIMENTS ON THE TROPICAL AIR-SEA INTERACTION WAVES |
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| Zhang Renhe and Chao Jiping. NUMERICAL EXPERIMENTS ON THE TROPICAL AIR-SEA INTERACTION WAVES[J]. Acta Meteorologica Sinica, 1992, 6(2): 148-158 |
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| Authors: | Zhang Renhe and Chao Jiping |
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| Affiliation: | Zhang Renhe Institute of Atmospheric Physics,Academia Sinica,Beijing 100080 Chao Jiping National Research Center for Marine Environmental Forecasts,State Oceanic Administration,Beijing 100081 |
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| Abstract: | By means of the numerical method,the tropical air-sea interaction waves are studied.The results show that when the Kelvin waves are filtered out and only the equatorial Rossby waves are reserved both in the atmosphere and in the ocean,the disturbances can also propagate eastward because of the air-sea interaction.The critical wavelength of the eastward propagating waves is related to the intensity of the air-sea interaction.The stronger the air-sea interaction,the larger the eastward propagating components of the air-sea interaction waves.The results of the numerical experiments are in good agreement with those of the theoretical analysis(Chao and Zhang,1988). |
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| Keywords: | equatorial Rossby waves Kelvin waves tropical air-sea interaction waves |
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