Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait
The global thermohaline circulation is an important part of Earth's climate system. Cold, dense water formed in the Nordic Seas enters the Atlantic Ocean as overflows across the sills of the Greenland-Scotland Ridge. The Denmark Strait Overflow (DSO) is one of the main sources of North Atlantic...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , |
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Language: | English |
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AGU (American Geophysical Union)
2005
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Online Access: | https://oceanrep.geomar.de/id/eprint/6614/ https://oceanrep.geomar.de/id/eprint/6614/1/2004GL021463.pdf https://doi.org/10.1029/2004GL021463 |
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ftoceanrep:oai:oceanrep.geomar.de:6614 2023-05-15T16:00:36+02:00 Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait Macrander, Andreas Send, Uwe Valdimarsson, H. Jonsson, S. Käse, Rolf H. 2005 text https://oceanrep.geomar.de/id/eprint/6614/ https://oceanrep.geomar.de/id/eprint/6614/1/2004GL021463.pdf https://doi.org/10.1029/2004GL021463 en eng AGU (American Geophysical Union) https://oceanrep.geomar.de/id/eprint/6614/1/2004GL021463.pdf Macrander, A., Send, U., Valdimarsson, H., Jonsson, S. and Käse, R. H. (2005) Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait. Open Access Geophysical Research Letters, 32 (5). L06606. DOI 10.1029/2004GL021463 <https://doi.org/10.1029/2004GL021463>. doi:10.1029/2004GL021463 info:eu-repo/semantics/openAccess Article PeerReviewed 2005 ftoceanrep https://doi.org/10.1029/2004GL021463 2023-04-07T14:53:12Z The global thermohaline circulation is an important part of Earth's climate system. Cold, dense water formed in the Nordic Seas enters the Atlantic Ocean as overflows across the sills of the Greenland-Scotland Ridge. The Denmark Strait Overflow (DSO) is one of the main sources of North Atlantic Deep Water. Until now the DSO has been believed to be stable on interannual timescales. Here, for the first time, evidence is presented from a 4-year program of observations showing that overflow transports in 1999/2000 were approximately 30% higher than previous estimates. Later, transports decreased remarkably during the observation period, coincident with a temporary temperature increase of about 0.5°C. Article in Journal/Newspaper Denmark Strait Greenland Greenland-Scotland Ridge Nordic Seas North Atlantic Deep Water North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Greenland Geophysical Research Letters 32 6 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
The global thermohaline circulation is an important part of Earth's climate system. Cold, dense water formed in the Nordic Seas enters the Atlantic Ocean as overflows across the sills of the Greenland-Scotland Ridge. The Denmark Strait Overflow (DSO) is one of the main sources of North Atlantic Deep Water. Until now the DSO has been believed to be stable on interannual timescales. Here, for the first time, evidence is presented from a 4-year program of observations showing that overflow transports in 1999/2000 were approximately 30% higher than previous estimates. Later, transports decreased remarkably during the observation period, coincident with a temporary temperature increase of about 0.5°C. |
format |
Article in Journal/Newspaper |
author |
Macrander, Andreas Send, Uwe Valdimarsson, H. Jonsson, S. Käse, Rolf H. |
spellingShingle |
Macrander, Andreas Send, Uwe Valdimarsson, H. Jonsson, S. Käse, Rolf H. Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait |
author_facet |
Macrander, Andreas Send, Uwe Valdimarsson, H. Jonsson, S. Käse, Rolf H. |
author_sort |
Macrander, Andreas |
title |
Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait |
title_short |
Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait |
title_full |
Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait |
title_fullStr |
Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait |
title_full_unstemmed |
Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait |
title_sort |
interannual changes in the overflow from the nordic seas into the atlantic ocean through the denmark strait |
publisher |
AGU (American Geophysical Union) |
publishDate |
2005 |
url |
https://oceanrep.geomar.de/id/eprint/6614/ https://oceanrep.geomar.de/id/eprint/6614/1/2004GL021463.pdf https://doi.org/10.1029/2004GL021463 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Denmark Strait Greenland Greenland-Scotland Ridge Nordic Seas North Atlantic Deep Water North Atlantic |
genre_facet |
Denmark Strait Greenland Greenland-Scotland Ridge Nordic Seas North Atlantic Deep Water North Atlantic |
op_relation |
https://oceanrep.geomar.de/id/eprint/6614/1/2004GL021463.pdf Macrander, A., Send, U., Valdimarsson, H., Jonsson, S. and Käse, R. H. (2005) Interannual changes in the overflow from the Nordic Seas into the Atlantic Ocean through the Denmark Strait. Open Access Geophysical Research Letters, 32 (5). L06606. DOI 10.1029/2004GL021463 <https://doi.org/10.1029/2004GL021463>. doi:10.1029/2004GL021463 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2004GL021463 |
container_title |
Geophysical Research Letters |
container_volume |
32 |
container_issue |
6 |
_version_ |
1766396595812696064 |