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)可鼓出10米之高。
,温度突
(
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)可鼓出10米之高。
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资源自动生成，部分未经过人工审核，其表达内容亦不代表本软件的观点；若发现问题，欢迎向我们指正。
