Surface freshening in the Arctic Ocean's Eurasian Basin : an apparent consequence of recent change in the wind-driven circulation
The article of record as published may be found at https://doi.org/10.1029/2011JC006975 Data collected by an autonomous ice-based observatory that drifted into the Eurasian Basin between April and November 2010 indicate that the upper ocean was appreciably fresher than in 2007 and 2008. Sea ice and...
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American Geophysical Union
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Online Access: | https://hdl.handle.net/10945/62437 |
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ftnavalpschool:oai:calhoun.nps.edu:10945/62437 2024-06-09T07:43:34+00:00 Surface freshening in the Arctic Ocean's Eurasian Basin : an apparent consequence of recent change in the wind-driven circulation Timmermans, Mary-Louise Proshutinsky, Andrey Krishfield, Richard A. Perovich, Donald K. Richter-Menge, Jackie A. Stanton, Timothy P. Toole, John M. 2011-07-23 application/pdf https://hdl.handle.net/10945/62437 en_US eng American Geophysical Union Journal of Geophysical Research 116 (2011): C00D03, doi:10.1029/2011JC006975. Journal of Geophysical Research 116 (2011): C00D03 https://hdl.handle.net/10945/62437 Arctic Ocean Circulation Fresh water Article 2011 ftnavalpschool https://doi.org/10.1029/2011JC006975 2024-05-15T00:44:17Z The article of record as published may be found at https://doi.org/10.1029/2011JC006975 Data collected by an autonomous ice-based observatory that drifted into the Eurasian Basin between April and November 2010 indicate that the upper ocean was appreciably fresher than in 2007 and 2008. Sea ice and snowmelt over the course of the 2010 drift amounted to an input of less than 0.5 m of liquid freshwater to the ocean (comparable to the freshening by melting estimated for those previous years), while the observed change in upper-ocean salinity over the melt period implies a freshwater gain of about 0.7 m. Results of a wind-driven ocean model corroborate the observations of freshening and suggest that unusually fresh surface waters observed in parts of the Eurasian Basin in 2010 may have been due to the spreading of anomalously fresh water previously residing in the Beaufort Gyre. This flux is likely associated with a 2009 shift in the large-scale atmospheric circulation to a significant reduction in strength of the anticyclonic Beaufort Gyre and the Transpolar Drift Stream. This work was funded by the National Science Foundation Office of Polar Programs Arctic Sciences Section under awards ARC‐0519899, ARC‐0856479, and ARC‐ 0806306. Article in Journal/Newspaper Arctic Arctic Ocean Arctic Sciences Section National Science Foundation Office of Polar Programs Sea ice Naval Postgraduate School: Calhoun Arctic Arctic Ocean Journal of Geophysical Research 116 |
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Open Polar |
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Naval Postgraduate School: Calhoun |
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ftnavalpschool |
language |
English |
topic |
Arctic Ocean Circulation Fresh water |
spellingShingle |
Arctic Ocean Circulation Fresh water Timmermans, Mary-Louise Proshutinsky, Andrey Krishfield, Richard A. Perovich, Donald K. Richter-Menge, Jackie A. Stanton, Timothy P. Toole, John M. Surface freshening in the Arctic Ocean's Eurasian Basin : an apparent consequence of recent change in the wind-driven circulation |
topic_facet |
Arctic Ocean Circulation Fresh water |
description |
The article of record as published may be found at https://doi.org/10.1029/2011JC006975 Data collected by an autonomous ice-based observatory that drifted into the Eurasian Basin between April and November 2010 indicate that the upper ocean was appreciably fresher than in 2007 and 2008. Sea ice and snowmelt over the course of the 2010 drift amounted to an input of less than 0.5 m of liquid freshwater to the ocean (comparable to the freshening by melting estimated for those previous years), while the observed change in upper-ocean salinity over the melt period implies a freshwater gain of about 0.7 m. Results of a wind-driven ocean model corroborate the observations of freshening and suggest that unusually fresh surface waters observed in parts of the Eurasian Basin in 2010 may have been due to the spreading of anomalously fresh water previously residing in the Beaufort Gyre. This flux is likely associated with a 2009 shift in the large-scale atmospheric circulation to a significant reduction in strength of the anticyclonic Beaufort Gyre and the Transpolar Drift Stream. This work was funded by the National Science Foundation Office of Polar Programs Arctic Sciences Section under awards ARC‐0519899, ARC‐0856479, and ARC‐ 0806306. |
format |
Article in Journal/Newspaper |
author |
Timmermans, Mary-Louise Proshutinsky, Andrey Krishfield, Richard A. Perovich, Donald K. Richter-Menge, Jackie A. Stanton, Timothy P. Toole, John M. |
author_facet |
Timmermans, Mary-Louise Proshutinsky, Andrey Krishfield, Richard A. Perovich, Donald K. Richter-Menge, Jackie A. Stanton, Timothy P. Toole, John M. |
author_sort |
Timmermans, Mary-Louise |
title |
Surface freshening in the Arctic Ocean's Eurasian Basin : an apparent consequence of recent change in the wind-driven circulation |
title_short |
Surface freshening in the Arctic Ocean's Eurasian Basin : an apparent consequence of recent change in the wind-driven circulation |
title_full |
Surface freshening in the Arctic Ocean's Eurasian Basin : an apparent consequence of recent change in the wind-driven circulation |
title_fullStr |
Surface freshening in the Arctic Ocean's Eurasian Basin : an apparent consequence of recent change in the wind-driven circulation |
title_full_unstemmed |
Surface freshening in the Arctic Ocean's Eurasian Basin : an apparent consequence of recent change in the wind-driven circulation |
title_sort |
surface freshening in the arctic ocean's eurasian basin : an apparent consequence of recent change in the wind-driven circulation |
publisher |
American Geophysical Union |
publishDate |
2011 |
url |
https://hdl.handle.net/10945/62437 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Arctic Sciences Section National Science Foundation Office of Polar Programs Sea ice |
genre_facet |
Arctic Arctic Ocean Arctic Sciences Section National Science Foundation Office of Polar Programs Sea ice |
op_relation |
Journal of Geophysical Research 116 (2011): C00D03, doi:10.1029/2011JC006975. Journal of Geophysical Research 116 (2011): C00D03 https://hdl.handle.net/10945/62437 |
op_doi |
https://doi.org/10.1029/2011JC006975 |
container_title |
Journal of Geophysical Research |
container_volume |
116 |
_version_ |
1801372403211698176 |