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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.

上升流使得局部温越层(温暖海交界层)可鼓出10米之高。

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

而厄尔尼诺发生的份,这样的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.

浮游生物需要养分,但几乎所有的养分都在海,因为水下约200的一层海水--温跃层的阻隔而无法到达海面。

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