Atlantic water flow through the Barents and Kara Seas
The pathway and transformation of water from the Norwegian Sea across the Barents Sea and through the St. Anna Trough are documented from hydrographic and current measurements of the 1990s. The transport through an array of moorings in the north-eastern Barents Sea was between 0.6 Sv in summer and 2...
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ftawi:oai:epic.awi.de:5657 2023-09-05T13:17:49+02:00 Atlantic water flow through the Barents and Kara Seas Schauer, Ursula Loeng, H. Rudels, B. Ozhigin, V. K. Dieck, Wolfgang 2002 https://epic.awi.de/id/eprint/5657/ https://hdl.handle.net/10013/epic.16220 unknown Schauer, U. , Loeng, H. , Rudels, B. , Ozhigin, V. K. and Dieck, W. (2002) Atlantic water flow through the Barents and Kara Seas , Deep-Sea Research I, 49, 12, pp., pp. 2281-2298 . hdl:10013/epic.16220 EPIC3Deep-Sea Research I, 49, 12, pp., pp. 2281-2298 Article isiRev 2002 ftawi 2023-08-22T19:45:33Z The pathway and transformation of water from the Norwegian Sea across the Barents Sea and through the St. Anna Trough are documented from hydrographic and current measurements of the 1990s. The transport through an array of moorings in the north-eastern Barents Sea was between 0.6 Sv in summer and 2.6 Sv in winter towards the Kara Sea and between zero and 0.3 Sv towards the Barents Sea with a record mean net flow of 1.5 Sv. The westward flow originates in the Fram Strait branch of Atlantic Water at the Eurasian continental slope, while the eastward flow constitutes the Barents Sea branch, continuing from the western Barents Sea opening.About 75% of the eastward flow was colder than 0°C. The flow was strongly sheared, with the highest velocities close to the bottom. A deep layer with almost constant temperature of about -0.5°C throughout the year formed about 50% of the flow to the Kara Sea. This water was a mixture between warm saline Atlantic Water and cold, brine-enriched water generated through freezing and convection in polynyas west of Novaya Zemlya, and possibly also at the Central Bank. Its salinity is lower than that of the Atlantic Water at its entrance to the Barents Sea, because the ice formation occurs in a low salinity surface layer. The released brine increases the salinity and density of the surface layer sufficiently for it to convect, but not necessarily above the salinity of the Atlantic Water. The fresh-water west of Novaya Zemlya primarily stems from continental runoff and at the Central Bank probably from ice melt. The amount of fresh water compares to about 22% of the terrestrial fresh water supply to the western Barents Sea. The deep layer continues to the Kara Sea without further change and enters the Nansen Basin at or below the core depth of the warm, saline Fram Strait branch. Because it is colder than 0°C it will not be addressed as Atlantic Water in the Arctic Ocean.In earlier decades, the Atlantic Water advected from Fram Strait was colder by almost 2K as compared to the 1990s, ... Article in Journal/Newspaper Arctic Barents Sea Fram Strait Kara Sea Nansen Nansen Basin Norwegian Sea Novaya Zemlya Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Arctic Barents Sea Kara Sea Norwegian Sea St. Anna Trough ENVELOPE(69.500,69.500,80.750,80.750) |
institution |
Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
The pathway and transformation of water from the Norwegian Sea across the Barents Sea and through the St. Anna Trough are documented from hydrographic and current measurements of the 1990s. The transport through an array of moorings in the north-eastern Barents Sea was between 0.6 Sv in summer and 2.6 Sv in winter towards the Kara Sea and between zero and 0.3 Sv towards the Barents Sea with a record mean net flow of 1.5 Sv. The westward flow originates in the Fram Strait branch of Atlantic Water at the Eurasian continental slope, while the eastward flow constitutes the Barents Sea branch, continuing from the western Barents Sea opening.About 75% of the eastward flow was colder than 0°C. The flow was strongly sheared, with the highest velocities close to the bottom. A deep layer with almost constant temperature of about -0.5°C throughout the year formed about 50% of the flow to the Kara Sea. This water was a mixture between warm saline Atlantic Water and cold, brine-enriched water generated through freezing and convection in polynyas west of Novaya Zemlya, and possibly also at the Central Bank. Its salinity is lower than that of the Atlantic Water at its entrance to the Barents Sea, because the ice formation occurs in a low salinity surface layer. The released brine increases the salinity and density of the surface layer sufficiently for it to convect, but not necessarily above the salinity of the Atlantic Water. The fresh-water west of Novaya Zemlya primarily stems from continental runoff and at the Central Bank probably from ice melt. The amount of fresh water compares to about 22% of the terrestrial fresh water supply to the western Barents Sea. The deep layer continues to the Kara Sea without further change and enters the Nansen Basin at or below the core depth of the warm, saline Fram Strait branch. Because it is colder than 0°C it will not be addressed as Atlantic Water in the Arctic Ocean.In earlier decades, the Atlantic Water advected from Fram Strait was colder by almost 2K as compared to the 1990s, ... |
format |
Article in Journal/Newspaper |
author |
Schauer, Ursula Loeng, H. Rudels, B. Ozhigin, V. K. Dieck, Wolfgang |
spellingShingle |
Schauer, Ursula Loeng, H. Rudels, B. Ozhigin, V. K. Dieck, Wolfgang Atlantic water flow through the Barents and Kara Seas |
author_facet |
Schauer, Ursula Loeng, H. Rudels, B. Ozhigin, V. K. Dieck, Wolfgang |
author_sort |
Schauer, Ursula |
title |
Atlantic water flow through the Barents and Kara Seas |
title_short |
Atlantic water flow through the Barents and Kara Seas |
title_full |
Atlantic water flow through the Barents and Kara Seas |
title_fullStr |
Atlantic water flow through the Barents and Kara Seas |
title_full_unstemmed |
Atlantic water flow through the Barents and Kara Seas |
title_sort |
atlantic water flow through the barents and kara seas |
publishDate |
2002 |
url |
https://epic.awi.de/id/eprint/5657/ https://hdl.handle.net/10013/epic.16220 |
long_lat |
ENVELOPE(69.500,69.500,80.750,80.750) |
geographic |
Arctic Barents Sea Kara Sea Norwegian Sea St. Anna Trough |
geographic_facet |
Arctic Barents Sea Kara Sea Norwegian Sea St. Anna Trough |
genre |
Arctic Barents Sea Fram Strait Kara Sea Nansen Nansen Basin Norwegian Sea Novaya Zemlya |
genre_facet |
Arctic Barents Sea Fram Strait Kara Sea Nansen Nansen Basin Norwegian Sea Novaya Zemlya |
op_source |
EPIC3Deep-Sea Research I, 49, 12, pp., pp. 2281-2298 |
op_relation |
Schauer, U. , Loeng, H. , Rudels, B. , Ozhigin, V. K. and Dieck, W. (2002) Atlantic water flow through the Barents and Kara Seas , Deep-Sea Research I, 49, 12, pp., pp. 2281-2298 . hdl:10013/epic.16220 |
_version_ |
1776198840265736192 |