摘要
简述了厄尔尼诺事件研究的最新进展 ,研究表明 :强潮汐加大垂直方向和水平方向海水的混合 ,将太平洋深层冷水翻上表面 (或使西部暖水流向东部 ) ,吸收 (或释放 )CO2 减弱 (或增强 )温室效应 ,使海洋上方空气变冷 (或变暖 ) ,产生拉尼娜冷事件 (或厄尔尼诺热事件 ) .海底火山活动亦受强潮汐的控制 .
Discussing some new advance on Einino in this paper. Strong tides increase the vertical and horizonal mixing of water in the oceans, drawing the cold/warm Pacific water from the depths/west to the surface/east, where it cools/warms the atmosphere above, absorbs/releases CO 2 to decrease/increase the greenhouse effect and makes La Nina/El Nino occur in the whole world. Volcano activities on the bottom of the sea are also controlled by strong tides, drawing warm water from the depths to the surface in the Pacific to control El Nino.
出处
《地球物理学进展》
CSCD
2002年第1期176-179,共4页
Progress in Geophysics
基金
国家自然科学基金项目 (4 97742 2 8)
