The Atlantic Water boundary current in the Nansen Basin : transport and mechanisms of lateral exchange
Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 121 (2016): 6946–6960, doi:10.1002/2016JC011715. Data...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/8577 2023-05-15T15:03:42+02:00 The Atlantic Water boundary current in the Nansen Basin : transport and mechanisms of lateral exchange Våge, Kjetil Pickart, Robert S. Pavlov, Vladimir Lin, Peigen Torres, Daniel J. Ingvaldsen, Randi B. Sundfjord, Arild Proshutinsky, Andrey 2016-09-22 https://hdl.handle.net/1912/8577 en eng John Wiley & Sons https://doi.org/10.1002/2016JC011715 Journal of Geophysical Research: Oceans 121 (2016): 6946–6960 https://hdl.handle.net/1912/8577 doi:10.1002/2016JC011715 Journal of Geophysical Research: Oceans 121 (2016): 6946–6960 doi:10.1002/2016JC011715 Atlantic Water Boundary current Nansen Basin Lateral exchange Eddy Upwelling Article 2016 ftwhoas https://doi.org/10.1002/2016JC011715 2022-05-28T22:59:48Z Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 121 (2016): 6946–6960, doi:10.1002/2016JC011715. Data from a shipboard hydrographic survey near 30°E in the Nansen Basin of the Arctic Ocean are used to investigate the structure and transport of the Atlantic Water boundary current. Two high-resolution synoptic crossings of the current indicate that it is roughly 30 km wide and weakly middepth-intensified. Using a previously determined definition of Atlantic Water, the transport of this water mass is calculated to be 1.6 ± 0.3 Sv, which is similar to the transport of Atlantic Water in the inner branch of the West Spitsbergen Current. At the time of the survey a small anticyclonic eddy of Atlantic Water was situated just offshore of the boundary current. The data suggest that the feature was recently detached from the boundary current, and, due to compensating effects of temperature and salinity on the thermal wind shear, the maximum swirl speed was situated below the hydrographic property core. Two other similar features were detected within our study domain, suggesting that these eddies are common and represent an effective means of fluxing warm and salty water from the boundary current into the interior. An atmospheric low-pressure system transiting south of our study area resulted in southeasterly winds prior to and during the field measurements. A comparison to hydrographic data from the Pacific Water boundary current in the Canada Basin under similar atmospheric forcing suggests that upwelling was taking place during the survey. This provides a second mechanism related to cross-stream exchange of heat and salt in this region of the Nansen Basin. Arctic Ocean program at the FRAM-High North Research Centre for Climate and the Environment; Steven Grossman Family Foundation; National Science Foundation Grant Number: ... Article in Journal/Newspaper Arctic Arctic Ocean canada basin Nansen Basin Spitsbergen Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Arctic Arctic Ocean Canada Pacific Journal of Geophysical Research: Oceans 121 9 6946 6960 |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Atlantic Water Boundary current Nansen Basin Lateral exchange Eddy Upwelling |
spellingShingle |
Atlantic Water Boundary current Nansen Basin Lateral exchange Eddy Upwelling Våge, Kjetil Pickart, Robert S. Pavlov, Vladimir Lin, Peigen Torres, Daniel J. Ingvaldsen, Randi B. Sundfjord, Arild Proshutinsky, Andrey The Atlantic Water boundary current in the Nansen Basin : transport and mechanisms of lateral exchange |
topic_facet |
Atlantic Water Boundary current Nansen Basin Lateral exchange Eddy Upwelling |
description |
Author Posting. © American Geophysical Union, 2016. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 121 (2016): 6946–6960, doi:10.1002/2016JC011715. Data from a shipboard hydrographic survey near 30°E in the Nansen Basin of the Arctic Ocean are used to investigate the structure and transport of the Atlantic Water boundary current. Two high-resolution synoptic crossings of the current indicate that it is roughly 30 km wide and weakly middepth-intensified. Using a previously determined definition of Atlantic Water, the transport of this water mass is calculated to be 1.6 ± 0.3 Sv, which is similar to the transport of Atlantic Water in the inner branch of the West Spitsbergen Current. At the time of the survey a small anticyclonic eddy of Atlantic Water was situated just offshore of the boundary current. The data suggest that the feature was recently detached from the boundary current, and, due to compensating effects of temperature and salinity on the thermal wind shear, the maximum swirl speed was situated below the hydrographic property core. Two other similar features were detected within our study domain, suggesting that these eddies are common and represent an effective means of fluxing warm and salty water from the boundary current into the interior. An atmospheric low-pressure system transiting south of our study area resulted in southeasterly winds prior to and during the field measurements. A comparison to hydrographic data from the Pacific Water boundary current in the Canada Basin under similar atmospheric forcing suggests that upwelling was taking place during the survey. This provides a second mechanism related to cross-stream exchange of heat and salt in this region of the Nansen Basin. Arctic Ocean program at the FRAM-High North Research Centre for Climate and the Environment; Steven Grossman Family Foundation; National Science Foundation Grant Number: ... |
format |
Article in Journal/Newspaper |
author |
Våge, Kjetil Pickart, Robert S. Pavlov, Vladimir Lin, Peigen Torres, Daniel J. Ingvaldsen, Randi B. Sundfjord, Arild Proshutinsky, Andrey |
author_facet |
Våge, Kjetil Pickart, Robert S. Pavlov, Vladimir Lin, Peigen Torres, Daniel J. Ingvaldsen, Randi B. Sundfjord, Arild Proshutinsky, Andrey |
author_sort |
Våge, Kjetil |
title |
The Atlantic Water boundary current in the Nansen Basin : transport and mechanisms of lateral exchange |
title_short |
The Atlantic Water boundary current in the Nansen Basin : transport and mechanisms of lateral exchange |
title_full |
The Atlantic Water boundary current in the Nansen Basin : transport and mechanisms of lateral exchange |
title_fullStr |
The Atlantic Water boundary current in the Nansen Basin : transport and mechanisms of lateral exchange |
title_full_unstemmed |
The Atlantic Water boundary current in the Nansen Basin : transport and mechanisms of lateral exchange |
title_sort |
atlantic water boundary current in the nansen basin : transport and mechanisms of lateral exchange |
publisher |
John Wiley & Sons |
publishDate |
2016 |
url |
https://hdl.handle.net/1912/8577 |
geographic |
Arctic Arctic Ocean Canada Pacific |
geographic_facet |
Arctic Arctic Ocean Canada Pacific |
genre |
Arctic Arctic Ocean canada basin Nansen Basin Spitsbergen |
genre_facet |
Arctic Arctic Ocean canada basin Nansen Basin Spitsbergen |
op_source |
Journal of Geophysical Research: Oceans 121 (2016): 6946–6960 doi:10.1002/2016JC011715 |
op_relation |
https://doi.org/10.1002/2016JC011715 Journal of Geophysical Research: Oceans 121 (2016): 6946–6960 https://hdl.handle.net/1912/8577 doi:10.1002/2016JC011715 |
op_doi |
https://doi.org/10.1002/2016JC011715 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
121 |
container_issue |
9 |
container_start_page |
6946 |
op_container_end_page |
6960 |
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1766335564355731456 |