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NUMERICAL STUDY OF SHORT TERM EFFECT OF SST ANOMALIES

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  • Using a 5-layer P-o mixed coordinates primitive equations model, a process of heavy rain is simulated that occurred over the middle-and lower-reaches of the Changjiang River on July 1-2, 1991 and numerical experiments are done of the effects of sea surface temperature (SST) anomalies over different waters on the precipitation. The result has shown that the appearance of SST anomaly is followed in a short term (2 or 3 days) by. A change in the pattern of circulation as well as in precipitation to some extent.
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    [2] Huang Ronghui, Lu Li, 1989. Numerical simulation of the relationship between the anomaly of subtropical high over East Asia and the convective activities in the western tropical Pacific. Adv. Atmos. Sci,6: 202-214.
    [3] Keshavamurty R N, 1982. Response of the atmosphere to sea surface temperature anomalies over the equatorial Pacific and the teleconnections of the southern oscillation. J Atmos. Sci., 39: 1241-1259.
    [4] Luo Shanhua, Jin Zuhui, Chen Lieting, 1985. Analysis of the correlation between SST in the Indian Ocean and the South China Sea and summer precipitation over the middle and lower reaches of the Changjiang River (in Chinese). Sci. Atmos. Sin., 9: 314-320.
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    [6] Ni Yunqi, Qian Yongfu, Lin Yuanbi, 1990. Influence of SST anomalies in the equatorial west Pacific and Indian Ocean on the summer monsoon in Asia (in Chinese). Sci. Meteor. Sin., 48: 336-343.
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Gu Jianfeng, Wang Qianqian, Liu Jiangang. NUMERICAL STUDY OF SHORT TERM EFFECT OF SST ANOMALIES [J]. Journal of Tropical Meteorology, 1999, 5(1): 17-23.
Gu Jianfeng, Wang Qianqian, Liu Jiangang. NUMERICAL STUDY OF SHORT TERM EFFECT OF SST ANOMALIES [J]. Journal of Tropical Meteorology, 1999, 5(1): 17-23.
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Manuscript History

Manuscript received: 28 July 1997
Manuscript revised: 26 March 1998
通讯作者: 陈斌, bchen63@163.com
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NUMERICAL STUDY OF SHORT TERM EFFECT OF SST ANOMALIES

Abstract: Using a 5-layer P-o mixed coordinates primitive equations model, a process of heavy rain is simulated that occurred over the middle-and lower-reaches of the Changjiang River on July 1-2, 1991 and numerical experiments are done of the effects of sea surface temperature (SST) anomalies over different waters on the precipitation. The result has shown that the appearance of SST anomaly is followed in a short term (2 or 3 days) by. A change in the pattern of circulation as well as in precipitation to some extent.

Gu Jianfeng, Wang Qianqian, Liu Jiangang. NUMERICAL STUDY OF SHORT TERM EFFECT OF SST ANOMALIES [J]. Journal of Tropical Meteorology, 1999, 5(1): 17-23.
Citation: Gu Jianfeng, Wang Qianqian, Liu Jiangang. NUMERICAL STUDY OF SHORT TERM EFFECT OF SST ANOMALIES [J]. Journal of Tropical Meteorology, 1999, 5(1): 17-23.
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