Atmospheric forcing of salinity in the overflow of Denmark Strait
The temporal evolution of the characteristics of Denmark Strait Overflow Water (DSOW) is reconstructed using hydrographic data and compared with possible atmospheric forcing mechanisms. It is concluded that the main factor influencing the DSOW characteristics at a time scale of one to several years...
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fttriple:oai:gotriple.eu:oai:doaj.org/article:0b9c1f98911a4b4d8f94e1be8e56ebf0 2023-05-15T16:00:34+02:00 Atmospheric forcing of salinity in the overflow of Denmark Strait J. Holfort T. Albrecht 2007-09-01 http://www.ocean-sci.net/3/411/2007/os-3-411-2007.pdf https://doaj.org/article/0b9c1f98911a4b4d8f94e1be8e56ebf0 en eng Copernicus Publications 1812-0784 1812-0792 http://www.ocean-sci.net/3/411/2007/os-3-411-2007.pdf https://doaj.org/article/0b9c1f98911a4b4d8f94e1be8e56ebf0 undefined Ocean Science, Vol 3, Iss 3, Pp 411-416 (2007) geo hist Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2007 fttriple 2023-01-22T18:59:35Z The temporal evolution of the characteristics of Denmark Strait Overflow Water (DSOW) is reconstructed using hydrographic data and compared with possible atmospheric forcing mechanisms. It is concluded that the main factor influencing the DSOW characteristics at a time scale of one to several years is the difference in mean sea level pressure across Denmark Strait or, in other words, the wind along Denmark Strait. At these time scales upstream changes in the characteristics of the different water masses involved in the formation of DSOW are only of minor importance. The main process responsible for the observed salinity changes in the DSOW is mixing in Denmark Strait. Triggered by the wind, different water masses contribute with changing amounts to the formation of DSOW, leading to the observed changes in the salinity of DSOW. Article in Journal/Newspaper Denmark Strait Unknown |
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geo hist |
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geo hist J. Holfort T. Albrecht Atmospheric forcing of salinity in the overflow of Denmark Strait |
topic_facet |
geo hist |
description |
The temporal evolution of the characteristics of Denmark Strait Overflow Water (DSOW) is reconstructed using hydrographic data and compared with possible atmospheric forcing mechanisms. It is concluded that the main factor influencing the DSOW characteristics at a time scale of one to several years is the difference in mean sea level pressure across Denmark Strait or, in other words, the wind along Denmark Strait. At these time scales upstream changes in the characteristics of the different water masses involved in the formation of DSOW are only of minor importance. The main process responsible for the observed salinity changes in the DSOW is mixing in Denmark Strait. Triggered by the wind, different water masses contribute with changing amounts to the formation of DSOW, leading to the observed changes in the salinity of DSOW. |
format |
Article in Journal/Newspaper |
author |
J. Holfort T. Albrecht |
author_facet |
J. Holfort T. Albrecht |
author_sort |
J. Holfort |
title |
Atmospheric forcing of salinity in the overflow of Denmark Strait |
title_short |
Atmospheric forcing of salinity in the overflow of Denmark Strait |
title_full |
Atmospheric forcing of salinity in the overflow of Denmark Strait |
title_fullStr |
Atmospheric forcing of salinity in the overflow of Denmark Strait |
title_full_unstemmed |
Atmospheric forcing of salinity in the overflow of Denmark Strait |
title_sort |
atmospheric forcing of salinity in the overflow of denmark strait |
publisher |
Copernicus Publications |
publishDate |
2007 |
url |
http://www.ocean-sci.net/3/411/2007/os-3-411-2007.pdf https://doaj.org/article/0b9c1f98911a4b4d8f94e1be8e56ebf0 |
genre |
Denmark Strait |
genre_facet |
Denmark Strait |
op_source |
Ocean Science, Vol 3, Iss 3, Pp 411-416 (2007) |
op_relation |
1812-0784 1812-0792 http://www.ocean-sci.net/3/411/2007/os-3-411-2007.pdf https://doaj.org/article/0b9c1f98911a4b4d8f94e1be8e56ebf0 |
op_rights |
undefined |
_version_ |
1766396559750070272 |