Directly measured currents and estimated transport pathways of Atlantic Water between 59.5°N and the Iceland–Faroes–Scotland Ridge
Using vessel-mounted acoustic Doppler current profiler data from four different routes between Scotland, Iceland and Greenland, we map out the mean flow of water in the top 400 m of the northeastern North Atlantic. The poleward transport east of the Reykjanes Ridge (RR) decreases from ~8.5 to 10 Sv...
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Stockholm University Press
2015
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Online Access: | https://doi.org/10.3402/tellusa.v67.28067 https://doaj.org/article/4d2f9d8022c644ba9b09b39b6f181534 |
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ftdoajarticles:oai:doaj.org/article:4d2f9d8022c644ba9b09b39b6f181534 2023-05-15T16:11:12+02:00 Directly measured currents and estimated transport pathways of Atlantic Water between 59.5°N and the Iceland–Faroes–Scotland Ridge Katelin H. Childers Charles N. Flagg Thomas Rossby Corinna Schrum 2015-11-01T00:00:00Z https://doi.org/10.3402/tellusa.v67.28067 https://doaj.org/article/4d2f9d8022c644ba9b09b39b6f181534 EN eng Stockholm University Press http://www.tellusa.net/index.php/tellusa/article/view/28067/pdf_62 https://doaj.org/toc/1600-0870 1600-0870 doi:10.3402/tellusa.v67.28067 https://doaj.org/article/4d2f9d8022c644ba9b09b39b6f181534 Tellus: Series A, Dynamic Meteorology and Oceanography, Vol 67, Iss 0, Pp 1-9 (2015) ADCP current measurements northeast Atlantic transport patterns repeat sampling from vessels in regular traffic Faroes–Shetland Channel Iceland–Faroes Ridge Oceanography GC1-1581 Meteorology. Climatology QC851-999 article 2015 ftdoajarticles https://doi.org/10.3402/tellusa.v67.28067 2022-12-30T23:53:08Z Using vessel-mounted acoustic Doppler current profiler data from four different routes between Scotland, Iceland and Greenland, we map out the mean flow of water in the top 400 m of the northeastern North Atlantic. The poleward transport east of the Reykjanes Ridge (RR) decreases from ~8.5 to 10 Sv (1 Sverdrup=106 m3 s−1) at 59.5°N to 61°N to 6 Sv crossing the Iceland–Faroes–Scotland Ridge. The two longest ~1200 km transport integrals have 1.4–0.94 Sv uncertainty, respectively. The overall decrease in transport can in large measure be accounted for by a ~1.5 Sv flow across the RR into the Irminger Sea north of 59.5°N and by a ~0.5 Sv overflow of dense water along the Iceland–Faroes Ridge. A remaining 0.5 Sv flux divergence is at the edge of detectability, but if real could be accounted for through wintertime convection to >400 m and densification of upper ocean water. The topography of the Iceland Basin and the banks west of Scotland play a fundamental role in controlling flow pathways towards and past Iceland, the Faroes and Scotland. Most water flows north unimpeded through the Iceland Basin, some in the centre of the basin along the Maury Channel, and some along Hatton Bank, turning east along the northern slopes of George Bligh Bank, Lousy Bank and Bill Bailey's Bank, whereupon the flow splits with ~3 Sv turning northwest towards the Iceland–Faroes Ridge and the remainder continuing east towards and north of the Wyville-Thomson Ridge (WTR) to the Scotland slope thereby increasing the Slope Current transport from ~1.5 Sv south of the WTR to 3.5 Sv in the Faroes–Shetland Channel. Article in Journal/Newspaper Faroes Greenland Iceland North Atlantic Northeast Atlantic Directory of Open Access Journals: DOAJ Articles Greenland Reykjanes ENVELOPE(-22.250,-22.250,65.467,65.467) Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054) Hatton Bank ENVELOPE(-18.000,-18.000,58.583,58.583) Wyville Thomson Ridge ENVELOPE(-7.500,-7.500,60.250,60.250) Wyville-Thomson Ridge ENVELOPE(-7.250,-7.250,60.000,60.000) Lousy Bank ENVELOPE(-12.583,-12.583,60.417,60.417) George Bligh Bank ENVELOPE(-13.667,-13.667,58.833,58.833) Bill Bailey's Bank ENVELOPE(-10.333,-10.333,60.583,60.583) Tellus A: Dynamic Meteorology and Oceanography 67 1 28067 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
ADCP current measurements northeast Atlantic transport patterns repeat sampling from vessels in regular traffic Faroes–Shetland Channel Iceland–Faroes Ridge Oceanography GC1-1581 Meteorology. Climatology QC851-999 |
spellingShingle |
ADCP current measurements northeast Atlantic transport patterns repeat sampling from vessels in regular traffic Faroes–Shetland Channel Iceland–Faroes Ridge Oceanography GC1-1581 Meteorology. Climatology QC851-999 Katelin H. Childers Charles N. Flagg Thomas Rossby Corinna Schrum Directly measured currents and estimated transport pathways of Atlantic Water between 59.5°N and the Iceland–Faroes–Scotland Ridge |
topic_facet |
ADCP current measurements northeast Atlantic transport patterns repeat sampling from vessels in regular traffic Faroes–Shetland Channel Iceland–Faroes Ridge Oceanography GC1-1581 Meteorology. Climatology QC851-999 |
description |
Using vessel-mounted acoustic Doppler current profiler data from four different routes between Scotland, Iceland and Greenland, we map out the mean flow of water in the top 400 m of the northeastern North Atlantic. The poleward transport east of the Reykjanes Ridge (RR) decreases from ~8.5 to 10 Sv (1 Sverdrup=106 m3 s−1) at 59.5°N to 61°N to 6 Sv crossing the Iceland–Faroes–Scotland Ridge. The two longest ~1200 km transport integrals have 1.4–0.94 Sv uncertainty, respectively. The overall decrease in transport can in large measure be accounted for by a ~1.5 Sv flow across the RR into the Irminger Sea north of 59.5°N and by a ~0.5 Sv overflow of dense water along the Iceland–Faroes Ridge. A remaining 0.5 Sv flux divergence is at the edge of detectability, but if real could be accounted for through wintertime convection to >400 m and densification of upper ocean water. The topography of the Iceland Basin and the banks west of Scotland play a fundamental role in controlling flow pathways towards and past Iceland, the Faroes and Scotland. Most water flows north unimpeded through the Iceland Basin, some in the centre of the basin along the Maury Channel, and some along Hatton Bank, turning east along the northern slopes of George Bligh Bank, Lousy Bank and Bill Bailey's Bank, whereupon the flow splits with ~3 Sv turning northwest towards the Iceland–Faroes Ridge and the remainder continuing east towards and north of the Wyville-Thomson Ridge (WTR) to the Scotland slope thereby increasing the Slope Current transport from ~1.5 Sv south of the WTR to 3.5 Sv in the Faroes–Shetland Channel. |
format |
Article in Journal/Newspaper |
author |
Katelin H. Childers Charles N. Flagg Thomas Rossby Corinna Schrum |
author_facet |
Katelin H. Childers Charles N. Flagg Thomas Rossby Corinna Schrum |
author_sort |
Katelin H. Childers |
title |
Directly measured currents and estimated transport pathways of Atlantic Water between 59.5°N and the Iceland–Faroes–Scotland Ridge |
title_short |
Directly measured currents and estimated transport pathways of Atlantic Water between 59.5°N and the Iceland–Faroes–Scotland Ridge |
title_full |
Directly measured currents and estimated transport pathways of Atlantic Water between 59.5°N and the Iceland–Faroes–Scotland Ridge |
title_fullStr |
Directly measured currents and estimated transport pathways of Atlantic Water between 59.5°N and the Iceland–Faroes–Scotland Ridge |
title_full_unstemmed |
Directly measured currents and estimated transport pathways of Atlantic Water between 59.5°N and the Iceland–Faroes–Scotland Ridge |
title_sort |
directly measured currents and estimated transport pathways of atlantic water between 59.5°n and the iceland–faroes–scotland ridge |
publisher |
Stockholm University Press |
publishDate |
2015 |
url |
https://doi.org/10.3402/tellusa.v67.28067 https://doaj.org/article/4d2f9d8022c644ba9b09b39b6f181534 |
long_lat |
ENVELOPE(-22.250,-22.250,65.467,65.467) ENVELOPE(-34.041,-34.041,63.054,63.054) ENVELOPE(-18.000,-18.000,58.583,58.583) ENVELOPE(-7.500,-7.500,60.250,60.250) ENVELOPE(-7.250,-7.250,60.000,60.000) ENVELOPE(-12.583,-12.583,60.417,60.417) ENVELOPE(-13.667,-13.667,58.833,58.833) ENVELOPE(-10.333,-10.333,60.583,60.583) |
geographic |
Greenland Reykjanes Irminger Sea Hatton Bank Wyville Thomson Ridge Wyville-Thomson Ridge Lousy Bank George Bligh Bank Bill Bailey's Bank |
geographic_facet |
Greenland Reykjanes Irminger Sea Hatton Bank Wyville Thomson Ridge Wyville-Thomson Ridge Lousy Bank George Bligh Bank Bill Bailey's Bank |
genre |
Faroes Greenland Iceland North Atlantic Northeast Atlantic |
genre_facet |
Faroes Greenland Iceland North Atlantic Northeast Atlantic |
op_source |
Tellus: Series A, Dynamic Meteorology and Oceanography, Vol 67, Iss 0, Pp 1-9 (2015) |
op_relation |
http://www.tellusa.net/index.php/tellusa/article/view/28067/pdf_62 https://doaj.org/toc/1600-0870 1600-0870 doi:10.3402/tellusa.v67.28067 https://doaj.org/article/4d2f9d8022c644ba9b09b39b6f181534 |
op_doi |
https://doi.org/10.3402/tellusa.v67.28067 |
container_title |
Tellus A: Dynamic Meteorology and Oceanography |
container_volume |
67 |
container_issue |
1 |
container_start_page |
28067 |
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1765996325468372992 |