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The depth of winter convection in the central Labrador Sea is strongly influenced by the prevailing stratification in late summer. For this late summer stratification salinity is as important as temperature, and in the upper water layers salinity even dominates. To analyze the source of the...
It is shown that the ocean’s hydrography occupies little volume in the three-dimensional space defined by salinity–temperature–pressure ( S –Θ– p ), and the implications of this observation for the mean vertical transport across density surfaces are discussed. Although ocean data have frequently...
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