赤道潜流 赤道潜流(Equatorial latent current) (Equatorial latent current) 南赤道流区下方温跃 南赤道流区下方温跃 层内，与赤道流相反自 层内，与赤道流相反自西向东的流，...
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流速矢量旋转谱水平随深度的变化呈马鞍形，低谷及深处的峰所在深度分别与南赤道流及赤道潜流的南边界所在深度大体一致。
The depths of the trough and the deeper peaks are almost coincident with those of the south boundaries of the South Equatorial Current and the Equatorial Undercurrent, respectively.
赤道西太平洋潜流和东太平洋南赤道流减弱是产生厄尔尼诺的必要条件。
It is necessary for the undercurrent to strongen in the western Pacific Ocean and for the sea surface current to weaken in the eastern Pacific Ocean.
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