Flow through Denmark Strait

On the basis of hydrographic observations taken in the vicinity of Denmark Strait, a primitive equation model is used to investigate physical mechanisms that control the exchange through the strait. The dense water transport is topographically controlled and predictions by Whitehead [1998] and Killw...

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Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Käse, Rolf H., Oschlies, Andreas
Format: Article in Journal/Newspaper
Language:English
Published: AGU (American Geophysical Union) 2000
Subjects:
Denmark Strait
Online Access:https://oceanrep.geomar.de/id/eprint/1888/
https://oceanrep.geomar.de/id/eprint/1888/1/Kase00.pdf
https://doi.org/10.1029/2000JC900111
id ftoceanrep:oai:oceanrep.geomar.de:1888
record_format openpolar
spelling ftoceanrep:oai:oceanrep.geomar.de:1888 2023-05-15T16:00:35+02:00 Flow through Denmark Strait Käse, Rolf H. Oschlies, Andreas 2000 text https://oceanrep.geomar.de/id/eprint/1888/ https://oceanrep.geomar.de/id/eprint/1888/1/Kase00.pdf https://doi.org/10.1029/2000JC900111 en eng AGU (American Geophysical Union) https://oceanrep.geomar.de/id/eprint/1888/1/Kase00.pdf Käse, R. H. and Oschlies, A. (2000) Flow through Denmark Strait. Open Access Journal of Geophysical Research: Oceans, 105 (C12). 28,527-28,546. DOI 10.1029/2000JC900111 <https://doi.org/10.1029/2000JC900111>. doi:10.1029/2000JC900111 cc_by_3.0 info:eu-repo/semantics/openAccess Article PeerReviewed 2000 ftoceanrep https://doi.org/10.1029/2000JC900111 2023-04-07T14:44:51Z On the basis of hydrographic observations taken in the vicinity of Denmark Strait, a primitive equation model is used to investigate physical mechanisms that control the exchange through the strait. The dense water transport is topographically controlled and predictions by Whitehead [1998] and Killworth and McDonald [1993] are consistent with numerical model results. The distribution of temperature and thickness of the modeled plume is in good agreement with the high-resolution hydrographic data. Article in Journal/Newspaper Denmark Strait OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Journal of Geophysical Research: Oceans 105 C12 28527 28546
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description On the basis of hydrographic observations taken in the vicinity of Denmark Strait, a primitive equation model is used to investigate physical mechanisms that control the exchange through the strait. The dense water transport is topographically controlled and predictions by Whitehead [1998] and Killworth and McDonald [1993] are consistent with numerical model results. The distribution of temperature and thickness of the modeled plume is in good agreement with the high-resolution hydrographic data.
format Article in Journal/Newspaper
author Käse, Rolf H.
Oschlies, Andreas
spellingShingle Käse, Rolf H.
Oschlies, Andreas
Flow through Denmark Strait
author_facet Käse, Rolf H.
Oschlies, Andreas
author_sort Käse, Rolf H.
title Flow through Denmark Strait
title_short Flow through Denmark Strait
title_full Flow through Denmark Strait
title_fullStr Flow through Denmark Strait
title_full_unstemmed Flow through Denmark Strait
title_sort flow through denmark strait
publisher AGU (American Geophysical Union)
publishDate 2000
url https://oceanrep.geomar.de/id/eprint/1888/
https://oceanrep.geomar.de/id/eprint/1888/1/Kase00.pdf
https://doi.org/10.1029/2000JC900111
genre Denmark Strait
genre_facet Denmark Strait
op_relation https://oceanrep.geomar.de/id/eprint/1888/1/Kase00.pdf
Käse, R. H. and Oschlies, A. (2000) Flow through Denmark Strait. Open Access Journal of Geophysical Research: Oceans, 105 (C12). 28,527-28,546. DOI 10.1029/2000JC900111 <https://doi.org/10.1029/2000JC900111>.
doi:10.1029/2000JC900111
op_rights cc_by_3.0
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1029/2000JC900111
container_title Journal of Geophysical Research: Oceans
container_volume 105
container_issue C12
container_start_page 28527
op_container_end_page 28546
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