赤道流是在赤道南、北的低纬度海域，自东向西流动的海流。
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棉兰老涡、赤道逆流和南赤道流存在较明显的年际变化。
Mindalao eddy, NECC and SEC were provided with obvious annual variation.
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.
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.
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