On the hydrography of Denmark Strait
Autor: | Hedinn Valdimarsson, Kjetil Våge, Kerstin Jochumsen, James B. Girton, Robert S. Pickart, Dana Mastropole |
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Rok vydání: | 2017 |
Předmět: |
Water mass
geography geography.geographical_feature_category 010504 meteorology & atmospheric sciences 010505 oceanography Oceanography 01 natural sciences Salinity Current (stream) Geophysics Water column Sill Space and Planetary Science Geochemistry and Petrology Earth and Planetary Sciences (miscellaneous) Hydrography Surface water Geology 0105 earth and related environmental sciences |
Zdroj: | Journal of Geophysical Research: Oceans. 122:306-321 |
ISSN: | 2169-9275 |
DOI: | 10.1002/2016jc012007 |
Popis: | Using 111 shipboard hydrographic sections across Denmark Strait occupied between 1990 and 2012, we characterize the mean conditions at the sill, quantify the water mass constituents, and describe the dominant features of the Denmark Strait Overflow Water (DSOW). The mean vertical sections of temperature, salinity, and density reveal the presence of circulation components found upstream of the sill, in particular the shelfbreak East Greenland Current (EGC) and the separated EGC. These correspond to hydrographic fronts consistent with surface-intensified southward flow. Deeper in the water column the isopycnals slope oppositely, indicative of bottom-intensified flow of DSOW. An end-member analysis indicates that the deepest part of Denmark Strait is dominated by Arctic-Origin Water with only small amounts of Atlantic-Origin Water. On the western side of the strait, the overflow water is a mixture of both constituents, with a contribution from Polar Surface Water. Weakly stratified “boluses” of dense water are present in 41% of the occupations, revealing that this is a common configuration of DSOW. The bolus water is primarily Arctic-Origin Water and constitutes the densest portion of the overflow. The boluses have become warmer and saltier over the 22 year record, which can be explained by changes in end-member properties and their relative contributions to bolus composition. |
Databáze: | OpenAIRE |
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