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The upwell ing brings the thermocline—the boundary layer between deep, cold water and the warm water of the surface—up as high as 30 feet from the top.

上升流使得局部(深处海水和表暖海水交界处)可鼓出10米之高。

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During an El Nino year, that thermocline tilt goes away.

而厄尔尼诺发份,这样温跃层就将不复存在。

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Plankton need nutrients, but most nutrients are locked in the deep, denied access to the surface by a layer of water called the thermocline, around 200 metres down.

浮游物需要,但几乎所有都在深海,因为水下约200米深处一层海水--温跃层阻隔而无法到达海面。

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