| The Latest Research Progress on El Ninod |
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| 作者姓名： | CHEN Dianyou WANG Ruiting and WANG Xudong |
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| 作者单位： | College of Geo-exploration Science and Technology，Jilin University，Changchun 130026，P.R. China |
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| 基金项目： | NationalNaturalScienceFundofChina，No .4 9774 2 2 8 |
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| 摘 要： | 1 ＭａｔｈｅｍａｔｉｃＭｏｄｅｌｏｆＴｉｄａｌＶｉｂｒａｔｉｏｎＳｕｐｐｏｓｅｔｈａｔ 3ｓｅｍｉ -ａｘｅｓｏｆａｅｌｌｉｐｓｏｉｄａｒｅａ ,ｂａｎｄｃ (ａ >ｂ >ｃ) ,ｌａｔｉｔｕｄｅｉｓθ ,ｌｏｎｇｉｔｕｄｅｉｓψ(ｃｈａｎｇｉｎｇｆｒｏｍ 0°ｔｏ 90°) ,
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The Latest Research Progress on El Ninod |
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| CHEN Dianyou,WANG Ruiting and WANG Xudong.The Latest Research Progress on El Ninod[J].Journal of Geoscientific Research in Northeast Asia,2002(2). |
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| Authors: | CHEN Dianyou WANG Ruiting and WANG Xudong |
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| Abstract: | Cold water in the deep Pacific can be drawn up to the surface (or west warm water drifts eastwards) because strong tide increases the mixing of seawater both in vertical and horizontal. In this way greenhouse effect is decreased or increased by means of absorbing (or releasing) CO 2 .Therefore, La Nina cold event (or El Nino warm event) may occur, which is caused by warming-up or cooling-down air above the ocean. Volcanic action at sea bottom is also controlled by strong tide. |
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| Keywords: | Differential rotation Tidal vibration and mixing El Nino event Volcanic action |
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