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(深处
冷海
和表面温暖海交界处层)可鼓
10
高。
面区与冷深冷区
层)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(深处冷海和表面温暖海交界处层)可鼓10高。
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