Labrador Sea freshening linked to Beaufort Gyre freshwater release
Abstract The Beaufort Gyre (BG), the largest Arctic Ocean freshwater reservoir, has drastically increased its liquid freshwater content by 40% in the past two decades. If released within a short period, the excess freshwater could potentially impact the large-scale ocean circulation by freshening th...
Published in: | Nature Communications |
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Online Access: | http://dx.doi.org/10.1038/s41467-021-21470-3 http://www.nature.com/articles/s41467-021-21470-3.pdf http://www.nature.com/articles/s41467-021-21470-3 |
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crspringernat:10.1038/s41467-021-21470-3 2023-05-15T14:28:50+02:00 Labrador Sea freshening linked to Beaufort Gyre freshwater release Zhang, Jiaxu Weijer, Wilbert Steele, Michael Cheng, Wei Verma, Tarun Veneziani, Milena United States Department of Commerce | NOAA | Climate Program Office DOE | Office of Science DOE | LDRD | Los Alamos National Laboratory United States Department of Defense | United States Navy | Office of Naval Research National Science Foundation 2021 http://dx.doi.org/10.1038/s41467-021-21470-3 http://www.nature.com/articles/s41467-021-21470-3.pdf http://www.nature.com/articles/s41467-021-21470-3 en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Nature Communications volume 12, issue 1 ISSN 2041-1723 General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry journal-article 2021 crspringernat https://doi.org/10.1038/s41467-021-21470-3 2022-01-04T16:44:13Z Abstract The Beaufort Gyre (BG), the largest Arctic Ocean freshwater reservoir, has drastically increased its liquid freshwater content by 40% in the past two decades. If released within a short period, the excess freshwater could potentially impact the large-scale ocean circulation by freshening the upper subpolar North Atlantic. Here, we track BG-sourced freshwater using passive tracers in a global ocean sea-ice model and show that this freshwater exited the Arctic mostly through the Canadian Arctic Archipelago, rather than Fram Strait, during an historical release event in 1983–1995. The Labrador Sea is the most affected region in the subpolar North Atlantic, with a freshening of 0.2 psu on the western shelves and 0.4 psu in the Labrador Current. Given that the present BG freshwater content anomaly is twice the historical analog studied here, the impact of a future rapid release on Labrador Sea salinity could be significant, easily exceeding similar fluxes from Greenland meltwater. Article in Journal/Newspaper Arctic Archipelago Arctic Arctic Ocean Canadian Arctic Archipelago Fram Strait Greenland Labrador Sea North Atlantic Sea ice Springer Nature (via Crossref) Arctic Arctic Ocean Canadian Arctic Archipelago Greenland Nature Communications 12 1 |
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Open Polar |
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Springer Nature (via Crossref) |
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crspringernat |
language |
English |
topic |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry |
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General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry Zhang, Jiaxu Weijer, Wilbert Steele, Michael Cheng, Wei Verma, Tarun Veneziani, Milena Labrador Sea freshening linked to Beaufort Gyre freshwater release |
topic_facet |
General Physics and Astronomy General Biochemistry, Genetics and Molecular Biology General Chemistry |
description |
Abstract The Beaufort Gyre (BG), the largest Arctic Ocean freshwater reservoir, has drastically increased its liquid freshwater content by 40% in the past two decades. If released within a short period, the excess freshwater could potentially impact the large-scale ocean circulation by freshening the upper subpolar North Atlantic. Here, we track BG-sourced freshwater using passive tracers in a global ocean sea-ice model and show that this freshwater exited the Arctic mostly through the Canadian Arctic Archipelago, rather than Fram Strait, during an historical release event in 1983–1995. The Labrador Sea is the most affected region in the subpolar North Atlantic, with a freshening of 0.2 psu on the western shelves and 0.4 psu in the Labrador Current. Given that the present BG freshwater content anomaly is twice the historical analog studied here, the impact of a future rapid release on Labrador Sea salinity could be significant, easily exceeding similar fluxes from Greenland meltwater. |
author2 |
United States Department of Commerce | NOAA | Climate Program Office DOE | Office of Science DOE | LDRD | Los Alamos National Laboratory United States Department of Defense | United States Navy | Office of Naval Research National Science Foundation |
format |
Article in Journal/Newspaper |
author |
Zhang, Jiaxu Weijer, Wilbert Steele, Michael Cheng, Wei Verma, Tarun Veneziani, Milena |
author_facet |
Zhang, Jiaxu Weijer, Wilbert Steele, Michael Cheng, Wei Verma, Tarun Veneziani, Milena |
author_sort |
Zhang, Jiaxu |
title |
Labrador Sea freshening linked to Beaufort Gyre freshwater release |
title_short |
Labrador Sea freshening linked to Beaufort Gyre freshwater release |
title_full |
Labrador Sea freshening linked to Beaufort Gyre freshwater release |
title_fullStr |
Labrador Sea freshening linked to Beaufort Gyre freshwater release |
title_full_unstemmed |
Labrador Sea freshening linked to Beaufort Gyre freshwater release |
title_sort |
labrador sea freshening linked to beaufort gyre freshwater release |
publisher |
Springer Science and Business Media LLC |
publishDate |
2021 |
url |
http://dx.doi.org/10.1038/s41467-021-21470-3 http://www.nature.com/articles/s41467-021-21470-3.pdf http://www.nature.com/articles/s41467-021-21470-3 |
geographic |
Arctic Arctic Ocean Canadian Arctic Archipelago Greenland |
geographic_facet |
Arctic Arctic Ocean Canadian Arctic Archipelago Greenland |
genre |
Arctic Archipelago Arctic Arctic Ocean Canadian Arctic Archipelago Fram Strait Greenland Labrador Sea North Atlantic Sea ice |
genre_facet |
Arctic Archipelago Arctic Arctic Ocean Canadian Arctic Archipelago Fram Strait Greenland Labrador Sea North Atlantic Sea ice |
op_source |
Nature Communications volume 12, issue 1 ISSN 2041-1723 |
op_rights |
https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s41467-021-21470-3 |
container_title |
Nature Communications |
container_volume |
12 |
container_issue |
1 |
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1766302978056126464 |