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The permanent Arctic halocline, one of the particular structures in the upper Arctic ocean, is very important to the maintenance of the sea ice and cold surface layer in the Arctic ocean.

长年存在的盐跃层是北冰洋上层洋独有的结构之一,对维持北冰洋表层的低温特冰存在起着非常重的作用。

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PBS地球-气候变幻

And it turns out that you can't grow sea ice over oceans that don't have a halocline.

事实证明,你不能在没有盐跃层的海洋海冰。

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PBS地球-气候变幻

So the fact that these layers don't mix and disrupt this halocline is super important to the global climate.

此,这些层不会混合这种盐跃层这一事实对全球气候非常重要。

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PBS地球-气候变幻

Usually cold water is denser and falls to the bottom, but in the Arctic, there's a strong halocline where saltier, denser water is at the bottom and freshwater is at the top.

通常冷水密度更大, 会落到底部,但在北极,有一个强烈的盐跃层,底部是咸度更高、密度更大的水, 而顶部是淡水。

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