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
越
(深处的
冷海水和表面的
暖海水交界处的水
)可鼓出10米之高。


,
度突变
(较热的水面区与冷的深冷水区之间的水
)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
越
(深处的
冷海水和表面的
暖海水交界处的水
)可鼓出10米之高。
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