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
(深处的
冷海水
的暖海水交界处的水)可鼓出10米之高。
跃
,度突变(较热的水
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(深处的冷海水的暖海水交界处的水)可鼓出10米之高。
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