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The Latest Research Progress on El Nino |
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| Authors: | CHEN Dianyou WANG Ruiting WANG Xudong |
| 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) CO2. Therefore, La Nina cold event (or El Nino warm event) may occur,which is caused by wanning - up or cooling - down air above the ocean. Volcanic action at sea bottom is also controlled by strong tide. |
| Keywords: | Differential rotation Tidal vibration and mixing El Nino event Volcanic action |
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