A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity

The Beaufort Gyre (BG) is a large anticyclonic circulation in the Arctic Ocean. Its strength is directly related to the halocline depth, and therefore also to the storage of freshwater. It has recently been proposed that the equilibrium state of the BG is set by the Ice-Ocean Governor, a negative fe...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Doddridge, Edward W., Meneghello, Gianluca, Marshall, John C., Scott, Jeffery R.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2020
Subjects:
Online Access:https://hdl.handle.net/1721.1/124772
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spelling ftmit:oai:dspace.mit.edu:1721.1/124772 2023-06-11T04:09:15+02:00 A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity Doddridge, Edward W. Meneghello, Gianluca Marshall, John C. Scott, Jeffery R. 2020-04-21T17:46:27Z application/pdf https://hdl.handle.net/1721.1/124772 en eng American Geophysical Union (AGU) 10.1029/2018JC014897 Journal of geophysical research: oceans 2169-9275 2169-9291 https://hdl.handle.net/1721.1/124772 Doddridge, Edward W., Gianluca Meneghello, John Marshall, and Jeffery Scott, "A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity." Journal of geophysical research: oceans 124, 5 (April 2019): p. 3107-24 doi 10.1029/2018JC014897 ©2019 Author(s) Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. MIT web domain Article http://purl.org/eprint/type/JournalArticle 2020 ftmit https://doi.org/10.1029/2018JC014897 2023-05-29T08:47:34Z The Beaufort Gyre (BG) is a large anticyclonic circulation in the Arctic Ocean. Its strength is directly related to the halocline depth, and therefore also to the storage of freshwater. It has recently been proposed that the equilibrium state of the BG is set by the Ice-Ocean Governor, a negative feedback between surface currents and ice-ocean stress, rather than a balance between lateral mesoscale eddy fluxes and surface Ekman pumping. However, mesoscale eddies are present in the Arctic Ocean; it is therefore important to extend the Ice-Ocean Governor theory to include lateral fluxes due to mesoscale eddies. Here, a nonlinear ordinary differential equation is derived that represents the effects of wind stress, the Ice-Ocean Governor, and eddy fluxes. Equilibrium and time-varying solutions to this three-way balance equation are obtained and shown to closely match the output from a hierarchy of numerical simulations, indicating that the analytical model represents the processes controlling BG equilibration. The equilibration timescale derived from this three-way balance is faster than the eddy equilibration timescale and slower than the Ice-Ocean Governor equilibration timescales for most values of eddy diffusivity. The sensitivity of the BG equilibrium depth to changes in eddy diffusivity and the presence of the Ice-Ocean Governor is also explored. These results show that predicting the response of the BG to changing surface forcing and sea ice conditions requires faithfully capturing the three-way balance between the Ice-Ocean Governor, wind stress, and eddy fluxes. ©2019 Article in Journal/Newspaper Arctic Arctic Ocean Sea ice DSpace@MIT (Massachusetts Institute of Technology) Arctic Arctic Ocean Journal of Geophysical Research: Oceans 124 5 3107 3124
institution Open Polar
collection DSpace@MIT (Massachusetts Institute of Technology)
op_collection_id ftmit
language English
description The Beaufort Gyre (BG) is a large anticyclonic circulation in the Arctic Ocean. Its strength is directly related to the halocline depth, and therefore also to the storage of freshwater. It has recently been proposed that the equilibrium state of the BG is set by the Ice-Ocean Governor, a negative feedback between surface currents and ice-ocean stress, rather than a balance between lateral mesoscale eddy fluxes and surface Ekman pumping. However, mesoscale eddies are present in the Arctic Ocean; it is therefore important to extend the Ice-Ocean Governor theory to include lateral fluxes due to mesoscale eddies. Here, a nonlinear ordinary differential equation is derived that represents the effects of wind stress, the Ice-Ocean Governor, and eddy fluxes. Equilibrium and time-varying solutions to this three-way balance equation are obtained and shown to closely match the output from a hierarchy of numerical simulations, indicating that the analytical model represents the processes controlling BG equilibration. The equilibration timescale derived from this three-way balance is faster than the eddy equilibration timescale and slower than the Ice-Ocean Governor equilibration timescales for most values of eddy diffusivity. The sensitivity of the BG equilibrium depth to changes in eddy diffusivity and the presence of the Ice-Ocean Governor is also explored. These results show that predicting the response of the BG to changing surface forcing and sea ice conditions requires faithfully capturing the three-way balance between the Ice-Ocean Governor, wind stress, and eddy fluxes. ©2019
format Article in Journal/Newspaper
author Doddridge, Edward W.
Meneghello, Gianluca
Marshall, John C.
Scott, Jeffery R.
spellingShingle Doddridge, Edward W.
Meneghello, Gianluca
Marshall, John C.
Scott, Jeffery R.
A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity
author_facet Doddridge, Edward W.
Meneghello, Gianluca
Marshall, John C.
Scott, Jeffery R.
author_sort Doddridge, Edward W.
title A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity
title_short A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity
title_full A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity
title_fullStr A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity
title_full_unstemmed A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity
title_sort three-way balance in the beaufort gyre: the ice-ocean governor, wind stress, and eddy diffusivity
publisher American Geophysical Union (AGU)
publishDate 2020
url https://hdl.handle.net/1721.1/124772
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_source MIT web domain
op_relation 10.1029/2018JC014897
Journal of geophysical research: oceans
2169-9275
2169-9291
https://hdl.handle.net/1721.1/124772
Doddridge, Edward W., Gianluca Meneghello, John Marshall, and Jeffery Scott, "A three-way balance in the Beaufort Gyre: the ice-ocean governor, wind stress, and eddy diffusivity." Journal of geophysical research: oceans 124, 5 (April 2019): p. 3107-24 doi 10.1029/2018JC014897 ©2019 Author(s)
op_rights Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
op_doi https://doi.org/10.1029/2018JC014897
container_title Journal of Geophysical Research: Oceans
container_volume 124
container_issue 5
container_start_page 3107
op_container_end_page 3124
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