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
(深处的
冷海水和表面的温暖海水交界处的水)
出10米之高。
,温度突变(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.
上升流使得局部温越(深处的冷海水和表面的温暖海水交界处的水)出10米之高。
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