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

The freshwater content of the Beaufort Gyre in the Western Arctic Ocean has increased in response to almost two decades of persistent anti-cyclonic winds. Here, the authors found that dramatic loss of sea ice and acceleration of surface currents after 2007 led to a net annual wind energy input to th...

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Autores principales:	Thomas W. K. Armitage, Georgy E. Manucharyan, Alek A. Petty, Ron Kwok, Andrew F. Thompson
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/711d5a04cc5a4030a0622691fc540fa5
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spelling	oai:doaj.org-article:711d5a04cc5a4030a0622691fc540fa52021-12-02T14:42:14ZEnhanced eddy activity in the Beaufort Gyre in response to sea ice loss10.1038/s41467-020-14449-z2041-1723https://doaj.org/article/711d5a04cc5a4030a0622691fc540fa52020-02-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-14449-zhttps://doaj.org/toc/2041-1723The freshwater content of the Beaufort Gyre in the Western Arctic Ocean has increased in response to almost two decades of persistent anti-cyclonic winds. Here, the authors found that dramatic loss of sea ice and acceleration of surface currents after 2007 led to a net annual wind energy input to the Beaufort Gyre, and anticipate that continued sea ice decline will lead to an increasingly energetic Beaufort Gyre.Thomas W. K. ArmitageGeorgy E. ManucharyanAlek A. PettyRon KwokAndrew F. ThompsonNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-8 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Thomas W. K. Armitage Georgy E. Manucharyan Alek A. Petty Ron Kwok Andrew F. Thompson Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss
description	The freshwater content of the Beaufort Gyre in the Western Arctic Ocean has increased in response to almost two decades of persistent anti-cyclonic winds. Here, the authors found that dramatic loss of sea ice and acceleration of surface currents after 2007 led to a net annual wind energy input to the Beaufort Gyre, and anticipate that continued sea ice decline will lead to an increasingly energetic Beaufort Gyre.
format	article
author	Thomas W. K. Armitage Georgy E. Manucharyan Alek A. Petty Ron Kwok Andrew F. Thompson
author_facet	Thomas W. K. Armitage Georgy E. Manucharyan Alek A. Petty Ron Kwok Andrew F. Thompson
author_sort	Thomas W. K. Armitage
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 Portfolio
publishDate	2020
url	https://doaj.org/article/711d5a04cc5a4030a0622691fc540fa5
work_keys_str_mv	AT thomaswkarmitage enhancededdyactivityinthebeaufortgyreinresponsetoseaiceloss AT georgyemanucharyan enhancededdyactivityinthebeaufortgyreinresponsetoseaiceloss AT alekapetty enhancededdyactivityinthebeaufortgyreinresponsetoseaiceloss AT ronkwok enhancededdyactivityinthebeaufortgyreinresponsetoseaiceloss AT andrewfthompson enhancededdyactivityinthebeaufortgyreinresponsetoseaiceloss
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Enhanced eddy activity in the Beaufort Gyre in response to sea ice loss

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