Seasonally derived components of the Canada Basin halocline
The Arctic halocline stratification is an important barrier to the transport of deep ocean heat to the underside of sea ice. Surface water in the Chukchi Sea, warmed in summer by solar radiation, ventilates the Canada Basin halocline to create a warm layer below the mixed‐layer base. The year‐round...
Published in: | Geophysical Research Letters |
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American Geophysical Union (AGU)
2017
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Online Access: | http://hdl.handle.net/1721.1/120078 |
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ftmit:oai:dspace.mit.edu:1721.1/120078 2023-06-11T04:09:02+02:00 Seasonally derived components of the Canada Basin halocline Timmermans, Mary-Louise Proshutinsky, Andrey Marshall, John C Scott, Jeffery R. Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Marshall, John Marshall, John C Scott, Jeffery R. 2017-02 application/pdf http://hdl.handle.net/1721.1/120078 en_US eng American Geophysical Union (AGU) http://dx.doi.org/10.1002/2017GL073042 Geophysical Research Letters 0094-8276 http://hdl.handle.net/1721.1/120078 Timmermans, Mary-Louise, John Marshall, Andrey Proshutinsky, and Jeffery Scott. “Seasonally Derived Components of the Canada Basin Halocline.” Geophysical Research Letters 44, no. 10 (May 26, 2017): 5008–5015. orcid:0000-0001-9230-3591 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. Prof. Marshall via Chris Sherratt Article http://purl.org/eprint/type/JournalArticle 2017 ftmit https://doi.org/10.1002/2017GL073042 2023-05-29T08:29:48Z The Arctic halocline stratification is an important barrier to the transport of deep ocean heat to the underside of sea ice. Surface water in the Chukchi Sea, warmed in summer by solar radiation, ventilates the Canada Basin halocline to create a warm layer below the mixed‐layer base. The year‐round persistence of this layer is shown to be consistent with the seasonal cycle of halocline ventilation. We present hydrographic observations and model results to show how Chukchi Sea density outcrops migrate seasonally as surface fluxes modify salinity and temperature. This migration is such that in winter, isopycnals bounding the warm halocline are blocked from ventilation, while the cool, relatively salty and deeper halocline layers are ventilated. In this way, the warm halocline is isolated by stratification (both vertically and laterally) each winter. Results shed light on the fate and impact to sea ice of the warm halocline under future freshening and warming of the surface Arctic Ocean. National Science Foundation (U.S.). Division of Polar Programs (Award 1350046) National Science Foundation (U.S.). Division of Polar Programs (Award 1603542) Article in Journal/Newspaper Arctic Arctic Ocean canada basin Chukchi Chukchi Sea Sea ice DSpace@MIT (Massachusetts Institute of Technology) Arctic Arctic Ocean Chukchi Sea Canada Geophysical Research Letters 44 10 5008 5015 |
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Open Polar |
collection |
DSpace@MIT (Massachusetts Institute of Technology) |
op_collection_id |
ftmit |
language |
English |
description |
The Arctic halocline stratification is an important barrier to the transport of deep ocean heat to the underside of sea ice. Surface water in the Chukchi Sea, warmed in summer by solar radiation, ventilates the Canada Basin halocline to create a warm layer below the mixed‐layer base. The year‐round persistence of this layer is shown to be consistent with the seasonal cycle of halocline ventilation. We present hydrographic observations and model results to show how Chukchi Sea density outcrops migrate seasonally as surface fluxes modify salinity and temperature. This migration is such that in winter, isopycnals bounding the warm halocline are blocked from ventilation, while the cool, relatively salty and deeper halocline layers are ventilated. In this way, the warm halocline is isolated by stratification (both vertically and laterally) each winter. Results shed light on the fate and impact to sea ice of the warm halocline under future freshening and warming of the surface Arctic Ocean. National Science Foundation (U.S.). Division of Polar Programs (Award 1350046) National Science Foundation (U.S.). Division of Polar Programs (Award 1603542) |
author2 |
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Marshall, John Marshall, John C Scott, Jeffery R. |
format |
Article in Journal/Newspaper |
author |
Timmermans, Mary-Louise Proshutinsky, Andrey Marshall, John C Scott, Jeffery R. |
spellingShingle |
Timmermans, Mary-Louise Proshutinsky, Andrey Marshall, John C Scott, Jeffery R. Seasonally derived components of the Canada Basin halocline |
author_facet |
Timmermans, Mary-Louise Proshutinsky, Andrey Marshall, John C Scott, Jeffery R. |
author_sort |
Timmermans, Mary-Louise |
title |
Seasonally derived components of the Canada Basin halocline |
title_short |
Seasonally derived components of the Canada Basin halocline |
title_full |
Seasonally derived components of the Canada Basin halocline |
title_fullStr |
Seasonally derived components of the Canada Basin halocline |
title_full_unstemmed |
Seasonally derived components of the Canada Basin halocline |
title_sort |
seasonally derived components of the canada basin halocline |
publisher |
American Geophysical Union (AGU) |
publishDate |
2017 |
url |
http://hdl.handle.net/1721.1/120078 |
geographic |
Arctic Arctic Ocean Chukchi Sea Canada |
geographic_facet |
Arctic Arctic Ocean Chukchi Sea Canada |
genre |
Arctic Arctic Ocean canada basin Chukchi Chukchi Sea Sea ice |
genre_facet |
Arctic Arctic Ocean canada basin Chukchi Chukchi Sea Sea ice |
op_source |
Prof. Marshall via Chris Sherratt |
op_relation |
http://dx.doi.org/10.1002/2017GL073042 Geophysical Research Letters 0094-8276 http://hdl.handle.net/1721.1/120078 Timmermans, Mary-Louise, John Marshall, Andrey Proshutinsky, and Jeffery Scott. “Seasonally Derived Components of the Canada Basin Halocline.” Geophysical Research Letters 44, no. 10 (May 26, 2017): 5008–5015. orcid:0000-0001-9230-3591 |
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/10.1002/2017GL073042 |
container_title |
Geophysical Research Letters |
container_volume |
44 |
container_issue |
10 |
container_start_page |
5008 |
op_container_end_page |
5015 |
_version_ |
1768382731553603584 |