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热盐环流
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热盐环流
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理学
热盐环流
释
thermohaline circulation
热盐环流
由于海洋表层受热冷却不均、蒸发降水不均所产生的温度和盐度变化,导致大洋海水密度分布不均匀而形成的海洋环流系统。与风生环流相比,热盐环流的流速较小,且活动区域主要集中在大洋的深层。
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