Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss

The Beaufort Gyre freshwater content has increased since the 1990s, potentially stabilizing in recent years. The mechanisms proposed to explain the stabilization involve either mesoscale eddy activity that opposes Ekman pumping or the reduction of Ekman pumping due to reduced sea ice–ocean surface...

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Published in:Nature Communications
Main Authors: Armitage, Thomas W. K., Manucharyan, Georgy E., Petty, Alek A., Kwok, Ron, Thompson, Andrew F.
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Publishing Group 2020
Subjects:
Online Access:https://doi.org/10.1038/s41467-020-14449-z
https://www.ncbi.nlm.nih.gov/pmc/PMC7005044
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spelling ftcaltechauth:oai:authors.library.caltech.edu:5k23p-vj216 2024-09-15T18:35:12+00:00 Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss Armitage, Thomas W. K. Manucharyan, Georgy E. Petty, Alek A. Kwok, Ron Thompson, Andrew F. 2020-02-06 https://doi.org/10.1038/s41467-020-14449-z https://www.ncbi.nlm.nih.gov/pmc/PMC7005044 unknown Nature Publishing Group https://doi.org/10.1038/s41467-020-14449-z oai:authors.library.caltech.edu:5k23p-vj216 https://www.ncbi.nlm.nih.gov/pmc/PMC7005044 eprintid:101240 resolverid:CaltechAUTHORS:20200212-104403401 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Nature Communications, 11, 761, (2020-02-06) Cryospheric science Physical oceanography info:eu-repo/semantics/article 2020 ftcaltechauth https://doi.org/10.1038/s41467-020-14449-z 2024-08-06T15:35:04Z The Beaufort Gyre freshwater content has increased since the 1990s, potentially stabilizing in recent years. The mechanisms proposed to explain the stabilization involve either mesoscale eddy activity that opposes Ekman pumping or the reduction of Ekman pumping due to reduced sea ice–ocean surface stress. However, the relative importance of these mechanisms is unclear. Here, we present observational estimates of the Beaufort Gyre mechanical energy budget and show that energy dissipation and freshwater content stabilization by eddies increased in the late-2000s. The loss of sea ice and acceleration of ocean currents after 2007 resulted in enhanced mechanical energy input but without corresponding increases in potential energy storage. To balance the energy surplus, eddy dissipation and its role in gyre stabilization must have increased after 2007. Our results imply that declining Arctic sea ice will lead to an increasingly energetic Beaufort Gyre with eddies playing a greater role in its stabilization. This is a U.S. government work and not under copyright protection in the U.S.; foreign copyright protection may apply 2020. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. Received 05 June 2018; Accepted 18 December 2019; Published 06 ... Article in Journal/Newspaper Sea ice Caltech Authors (California Institute of Technology) Nature Communications 11 1
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
topic Cryospheric science
Physical oceanography
spellingShingle Cryospheric science
Physical oceanography
Armitage, Thomas W. K.
Manucharyan, Georgy E.
Petty, Alek A.
Kwok, Ron
Thompson, Andrew F.
Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss
topic_facet Cryospheric science
Physical oceanography
description The Beaufort Gyre freshwater content has increased since the 1990s, potentially stabilizing in recent years. The mechanisms proposed to explain the stabilization involve either mesoscale eddy activity that opposes Ekman pumping or the reduction of Ekman pumping due to reduced sea ice–ocean surface stress. However, the relative importance of these mechanisms is unclear. Here, we present observational estimates of the Beaufort Gyre mechanical energy budget and show that energy dissipation and freshwater content stabilization by eddies increased in the late-2000s. The loss of sea ice and acceleration of ocean currents after 2007 resulted in enhanced mechanical energy input but without corresponding increases in potential energy storage. To balance the energy surplus, eddy dissipation and its role in gyre stabilization must have increased after 2007. Our results imply that declining Arctic sea ice will lead to an increasingly energetic Beaufort Gyre with eddies playing a greater role in its stabilization. This is a U.S. government work and not under copyright protection in the U.S.; foreign copyright protection may apply 2020. This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. Received 05 June 2018; Accepted 18 December 2019; Published 06 ...
format Article in Journal/Newspaper
author Armitage, Thomas W. K.
Manucharyan, Georgy E.
Petty, Alek A.
Kwok, Ron
Thompson, Andrew F.
author_facet Armitage, Thomas W. K.
Manucharyan, Georgy E.
Petty, Alek A.
Kwok, Ron
Thompson, Andrew F.
author_sort Armitage, Thomas W. K.
title Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss
title_short Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss
title_full Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss
title_fullStr Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss
title_full_unstemmed Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss
title_sort enhanced eddy activity in the beaufort gyre in response to sea ice loss
publisher Nature Publishing Group
publishDate 2020
url https://doi.org/10.1038/s41467-020-14449-z
https://www.ncbi.nlm.nih.gov/pmc/PMC7005044
genre Sea ice
genre_facet Sea ice
op_source Nature Communications, 11, 761, (2020-02-06)
op_relation https://doi.org/10.1038/s41467-020-14449-z
oai:authors.library.caltech.edu:5k23p-vj216
https://www.ncbi.nlm.nih.gov/pmc/PMC7005044
eprintid:101240
resolverid:CaltechAUTHORS:20200212-104403401
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.1038/s41467-020-14449-z
container_title Nature Communications
container_volume 11
container_issue 1
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