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Evolution Of North Atlantic Water Masses Inferred From Labrador Sea Salinity Series

机译:从拉布拉多海盐度系列推断北大西洋水团的演变

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摘要

The Labrador Sea is the coldest and freshest basin of the North Atlantic. Winter cooling in this sea produces Labrador Sea Water. This intermediate water plays an important role in the exchange of heat, freshwater, and other substances between the atmosphere and the abyssal ocean, affecting the water masses, circulation, and, ultimately, climate of the subpolar North Atlantic basins. The subpolar gyre of the North Atlantic has exhibited large changes in temperature, salinity, and volume over the past six decades, largely in response to changing winter conditions over the Labrador Sea. The signature of these changes can be seen in the lower limb of the Meridional Overturning Circulation down into the North Atlantic tropics.
机译:拉布拉多海是北大西洋最冷,最新鲜的盆地。该海中的冬季降温会产生拉布拉多海水。这种中间水在大气和深海之间的热,淡水和其他物质的交换中起着重要作用,影响水量,循环以及北极亚极盆地的气候。在过去的六十年中,北大西洋的亚极回旋显示了温度,盐度和体积的巨大变化,这主要是由于拉布拉多海冬季条件的变化。这些变化的特征可以在北大西洋热带的子午翻转环流的下肢看到。

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