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(深处的冷海水和表面的温暖海水交界处的水层)可鼓出10米之高。
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(深处的冷海水和表面的温暖海水交界处的水层)可鼓出10米之高。
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