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
和表面的温暖海交界处的)
鼓出10米之高。
,温度突变(较热的
面区与冷的深冷区之间的)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(深处的冷海和表面的温暖海交界处的)鼓出10米之高。
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