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 s...

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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: Text
Language:English
Published: Nature Publishing Group UK 2020
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7005044/
http://www.ncbi.nlm.nih.gov/pubmed/32029737
https://doi.org/10.1038/s41467-020-14449-z
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spelling ftpubmed:oai:pubmedcentral.nih.gov:7005044 2023-05-15T15:02:51+02:00 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 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7005044/ http://www.ncbi.nlm.nih.gov/pubmed/32029737 https://doi.org/10.1038/s41467-020-14449-z en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7005044/ http://www.ncbi.nlm.nih.gov/pubmed/32029737 http://dx.doi.org/10.1038/s41467-020-14449-z © This is a U.S. government work and not under copyright protection in the U.S.; foreign copyright protection may apply 2020 Open Access 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/. CC-BY Article Text 2020 ftpubmed https://doi.org/10.1038/s41467-020-14449-z 2020-02-16T01:29:27Z 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. Text Arctic Sea ice PubMed Central (PMC) Arctic Nature Communications 11 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
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 Article
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.
format Text
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 UK
publishDate 2020
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7005044/
http://www.ncbi.nlm.nih.gov/pubmed/32029737
https://doi.org/10.1038/s41467-020-14449-z
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7005044/
http://www.ncbi.nlm.nih.gov/pubmed/32029737
http://dx.doi.org/10.1038/s41467-020-14449-z
op_rights © This is a U.S. government work and not under copyright protection in the U.S.; foreign copyright protection may apply 2020
Open Access 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/.
op_rightsnorm CC-BY
op_doi https://doi.org/10.1038/s41467-020-14449-z
container_title Nature Communications
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