The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow
Dense water from the Nordic Seas passes through the Faroe Bank Channel and supplies the lower limb of the Atlantic Meridional Overturning Circulation, a critical component of the climate system. Yet, the upstream pathways of this water are not fully known. Here we present evidence of a previously un...
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ftpubmed:oai:pubmedcentral.nih.gov:7585422 2023-05-15T16:00:39+02:00 The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow Semper, Stefanie Pickart, Robert S. Våge, Kjetil Larsen, Karin Margretha H. Hátún, Hjálmar Hansen, Bogi 2020-10-23 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7585422/ http://www.ncbi.nlm.nih.gov/pubmed/33097704 https://doi.org/10.1038/s41467-020-19049-5 en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7585422/ http://www.ncbi.nlm.nih.gov/pubmed/33097704 http://dx.doi.org/10.1038/s41467-020-19049-5 © The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. CC-BY Nat Commun Article Text 2020 ftpubmed https://doi.org/10.1038/s41467-020-19049-5 2020-11-01T01:53:40Z Dense water from the Nordic Seas passes through the Faroe Bank Channel and supplies the lower limb of the Atlantic Meridional Overturning Circulation, a critical component of the climate system. Yet, the upstream pathways of this water are not fully known. Here we present evidence of a previously unrecognised deep current following the slope from Iceland toward the Faroe Bank Channel using high-resolution, synoptic shipboard observations and long-term measurements north of the Faroe Islands. The bulk of the volume transport of the current, named the Iceland-Faroe Slope Jet (IFSJ), is relatively uniform in hydrographic properties, very similar to the North Icelandic Jet flowing westward along the slope north of Iceland toward Denmark Strait. This suggests a common source for the two major overflows across the Greenland-Scotland Ridge. The IFSJ can account for approximately half of the total overflow transport through the Faroe Bank Channel, thus constituting a significant component of the overturning circulation in the Nordic Seas. Text Denmark Strait Faroe Islands Greenland Greenland-Scotland Ridge Iceland Nordic Seas PubMed Central (PMC) Faroe Bank ENVELOPE(-8.667,-8.667,60.917,60.917) Faroe Islands Greenland Nature Communications 11 1 |
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Article Semper, Stefanie Pickart, Robert S. Våge, Kjetil Larsen, Karin Margretha H. Hátún, Hjálmar Hansen, Bogi The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow |
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Article |
description |
Dense water from the Nordic Seas passes through the Faroe Bank Channel and supplies the lower limb of the Atlantic Meridional Overturning Circulation, a critical component of the climate system. Yet, the upstream pathways of this water are not fully known. Here we present evidence of a previously unrecognised deep current following the slope from Iceland toward the Faroe Bank Channel using high-resolution, synoptic shipboard observations and long-term measurements north of the Faroe Islands. The bulk of the volume transport of the current, named the Iceland-Faroe Slope Jet (IFSJ), is relatively uniform in hydrographic properties, very similar to the North Icelandic Jet flowing westward along the slope north of Iceland toward Denmark Strait. This suggests a common source for the two major overflows across the Greenland-Scotland Ridge. The IFSJ can account for approximately half of the total overflow transport through the Faroe Bank Channel, thus constituting a significant component of the overturning circulation in the Nordic Seas. |
format |
Text |
author |
Semper, Stefanie Pickart, Robert S. Våge, Kjetil Larsen, Karin Margretha H. Hátún, Hjálmar Hansen, Bogi |
author_facet |
Semper, Stefanie Pickart, Robert S. Våge, Kjetil Larsen, Karin Margretha H. Hátún, Hjálmar Hansen, Bogi |
author_sort |
Semper, Stefanie |
title |
The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow |
title_short |
The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow |
title_full |
The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow |
title_fullStr |
The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow |
title_full_unstemmed |
The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow |
title_sort |
iceland-faroe slope jet: a conduit for dense water toward the faroe bank channel overflow |
publisher |
Nature Publishing Group UK |
publishDate |
2020 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7585422/ http://www.ncbi.nlm.nih.gov/pubmed/33097704 https://doi.org/10.1038/s41467-020-19049-5 |
long_lat |
ENVELOPE(-8.667,-8.667,60.917,60.917) |
geographic |
Faroe Bank Faroe Islands Greenland |
geographic_facet |
Faroe Bank Faroe Islands Greenland |
genre |
Denmark Strait Faroe Islands Greenland Greenland-Scotland Ridge Iceland Nordic Seas |
genre_facet |
Denmark Strait Faroe Islands Greenland Greenland-Scotland Ridge Iceland Nordic Seas |
op_source |
Nat Commun |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7585422/ http://www.ncbi.nlm.nih.gov/pubmed/33097704 http://dx.doi.org/10.1038/s41467-020-19049-5 |
op_rights |
© The Author(s) 2020 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s41467-020-19049-5 |
container_title |
Nature Communications |
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11 |
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1 |
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