Structure and variability of the Denmark Strait Overflow: Model and observations
We report on a combined modeling and observational effort to understand the Denmark Strait Overflow (DSO). Four cruises over the course of 3 years mapped hydrographic properties and velocity fields with high spatial resolution. The observations reveal the mean path of the dense water, as well as the...
Published in: | Journal of Geophysical Research |
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Language: | English |
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Online Access: | https://oceanrep.geomar.de/id/eprint/2224/ https://oceanrep.geomar.de/id/eprint/2224/1/Kase03.pdf https://doi.org/10.1029/2002JC001548 |
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ftoceanrep:oai:oceanrep.geomar.de:2224 2023-05-15T16:00:37+02:00 Structure and variability of the Denmark Strait Overflow: Model and observations Käse, Rolf H. Girton, J. B. Sanford, T. B. 2003 text https://oceanrep.geomar.de/id/eprint/2224/ https://oceanrep.geomar.de/id/eprint/2224/1/Kase03.pdf https://doi.org/10.1029/2002JC001548 en eng AGU (American Geophysical Union) https://oceanrep.geomar.de/id/eprint/2224/1/Kase03.pdf Käse, R. H., Girton, J. B. and Sanford, T. B. (2003) Structure and variability of the Denmark Strait Overflow: Model and observations. Open Access Journal of Geophysical Research: Oceans, 108 (C6). p. 3181. DOI 10.1029/2002JC001548 <https://doi.org/10.1029/2002JC001548>. doi:10.1029/2002JC001548 cc_by_3.0 info:eu-repo/semantics/openAccess Article PeerReviewed 2003 ftoceanrep https://doi.org/10.1029/2002JC001548 2023-04-07T14:45:26Z We report on a combined modeling and observational effort to understand the Denmark Strait Overflow (DSO). Four cruises over the course of 3 years mapped hydrographic properties and velocity fields with high spatial resolution. The observations reveal the mean path of the dense water, as well as the presence of strong barotropic flows, energetic variability, and strong bottom friction and entrainment. A regional sigma coordinate numerical model of interbasin exchange using realistic bottom topography and an overflow forced only by an upstream reservoir of dense fluid is compared with the observations and used to further investigate these processes. The model successfully reproduces the volume transport of dense water at the sill, as well as the 1000-m descent of the dense water in the first 200 km from the sill and the intense eddies generated at 1–3 day intervals. Hydraulic control of the mean flow is indicated by a region supercritical to long gravity waves in the dense layer located approximately 100 km downstream of the sill in both model and observations. In addition, despite the differences in surface forcing, both model and observations exhibit similar transitions from mostly barotropic flow at the sill to a bottom-trapped baroclinic flow downstream, indicating the dominant role of the overflow in determining the full water column dynamics. Article in Journal/Newspaper Denmark Strait OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Journal of Geophysical Research 108 C6 |
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Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
We report on a combined modeling and observational effort to understand the Denmark Strait Overflow (DSO). Four cruises over the course of 3 years mapped hydrographic properties and velocity fields with high spatial resolution. The observations reveal the mean path of the dense water, as well as the presence of strong barotropic flows, energetic variability, and strong bottom friction and entrainment. A regional sigma coordinate numerical model of interbasin exchange using realistic bottom topography and an overflow forced only by an upstream reservoir of dense fluid is compared with the observations and used to further investigate these processes. The model successfully reproduces the volume transport of dense water at the sill, as well as the 1000-m descent of the dense water in the first 200 km from the sill and the intense eddies generated at 1–3 day intervals. Hydraulic control of the mean flow is indicated by a region supercritical to long gravity waves in the dense layer located approximately 100 km downstream of the sill in both model and observations. In addition, despite the differences in surface forcing, both model and observations exhibit similar transitions from mostly barotropic flow at the sill to a bottom-trapped baroclinic flow downstream, indicating the dominant role of the overflow in determining the full water column dynamics. |
format |
Article in Journal/Newspaper |
author |
Käse, Rolf H. Girton, J. B. Sanford, T. B. |
spellingShingle |
Käse, Rolf H. Girton, J. B. Sanford, T. B. Structure and variability of the Denmark Strait Overflow: Model and observations |
author_facet |
Käse, Rolf H. Girton, J. B. Sanford, T. B. |
author_sort |
Käse, Rolf H. |
title |
Structure and variability of the Denmark Strait Overflow: Model and observations |
title_short |
Structure and variability of the Denmark Strait Overflow: Model and observations |
title_full |
Structure and variability of the Denmark Strait Overflow: Model and observations |
title_fullStr |
Structure and variability of the Denmark Strait Overflow: Model and observations |
title_full_unstemmed |
Structure and variability of the Denmark Strait Overflow: Model and observations |
title_sort |
structure and variability of the denmark strait overflow: model and observations |
publisher |
AGU (American Geophysical Union) |
publishDate |
2003 |
url |
https://oceanrep.geomar.de/id/eprint/2224/ https://oceanrep.geomar.de/id/eprint/2224/1/Kase03.pdf https://doi.org/10.1029/2002JC001548 |
genre |
Denmark Strait |
genre_facet |
Denmark Strait |
op_relation |
https://oceanrep.geomar.de/id/eprint/2224/1/Kase03.pdf Käse, R. H., Girton, J. B. and Sanford, T. B. (2003) Structure and variability of the Denmark Strait Overflow: Model and observations. Open Access Journal of Geophysical Research: Oceans, 108 (C6). p. 3181. DOI 10.1029/2002JC001548 <https://doi.org/10.1029/2002JC001548>. doi:10.1029/2002JC001548 |
op_rights |
cc_by_3.0 info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2002JC001548 |
container_title |
Journal of Geophysical Research |
container_volume |
108 |
container_issue |
C6 |
_version_ |
1766396625554505728 |