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Between the devil and the deep blue sea: the role of the Amundsen Sea continental shelf in exchanges between ocean and ice shelves

Between the devil and the deep blue sea: the role of the Amundsen Sea continental shelf in exchanges between ocean and ice shelves
Between the devil and the deep blue sea: the role of the Amundsen Sea continental shelf in exchanges between ocean and ice shelves
The Amundsen Sea is a key region of Antarctica where ocean, atmosphere, sea ice, and ice sheet interact. For much of Antarctica, the relatively warm water of the open Southern Ocean (a few degrees above freezing) does not reach the Antarctic continental shelf in large volumes under current climate conditions. However, in the Amundsen Sea, warm water penetrates onto the continental shelf and provides heat that can melt the underside of the area’s floating ice shelves, thinning them. Here, we discuss how the ocean’s role in melting has come under increased scrutiny, present 2014 observations from the Amundsen Sea, and discuss their implications, highlighting aspects where understanding is still incomplete.
1042-8275
118-129
Heywood, Karen
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Biddle, Louise
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Boehme, Lars
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Dutrieux, Pierre
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Fedak, Michael
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Jenkins, Adrian
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Jones, Richard
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Kaiser, Jan
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Mallett, Helen
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Naveira Garabato, Alberto
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Renfrew, Ian
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Stevens, David
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Webber, Benjamin
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Heywood, Karen
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Biddle, Louise
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Boehme, Lars
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Dutrieux, Pierre
366b1813-3d70-4202-aabb-0e314e3d99b7
Fedak, Michael
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Jenkins, Adrian
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Jones, Richard
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Kaiser, Jan
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Mallett, Helen
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Naveira Garabato, Alberto
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Renfrew, Ian
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Stevens, David
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Webber, Benjamin
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Heywood, Karen, Biddle, Louise, Boehme, Lars, Dutrieux, Pierre, Fedak, Michael, Jenkins, Adrian, Jones, Richard, Kaiser, Jan, Mallett, Helen, Naveira Garabato, Alberto, Renfrew, Ian, Stevens, David and Webber, Benjamin (2016) Between the devil and the deep blue sea: the role of the Amundsen Sea continental shelf in exchanges between ocean and ice shelves. Oceanography, 29 (4), 118-129. (doi:10.5670/oceanog.2016.104).

Record type: Article

Abstract

The Amundsen Sea is a key region of Antarctica where ocean, atmosphere, sea ice, and ice sheet interact. For much of Antarctica, the relatively warm water of the open Southern Ocean (a few degrees above freezing) does not reach the Antarctic continental shelf in large volumes under current climate conditions. However, in the Amundsen Sea, warm water penetrates onto the continental shelf and provides heat that can melt the underside of the area’s floating ice shelves, thinning them. Here, we discuss how the ocean’s role in melting has come under increased scrutiny, present 2014 observations from the Amundsen Sea, and discuss their implications, highlighting aspects where understanding is still incomplete.

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Published date: December 2016
Organisations: Physical Oceanography

Identifiers

Local EPrints ID: 404902
URI: http://eprints.soton.ac.uk/id/eprint/404902
ISSN: 1042-8275
PURE UUID: 489cab20-1330-4a8c-8020-ff205694781d
ORCID for Alberto Naveira Garabato: ORCID iD orcid.org/0000-0001-6071-605X

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Date deposited: 18 Jan 2017 16:35
Last modified: 16 Mar 2024 03:48

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Contributors

Author: Karen Heywood
Author: Louise Biddle
Author: Lars Boehme
Author: Pierre Dutrieux
Author: Michael Fedak
Author: Adrian Jenkins
Author: Richard Jones
Author: Jan Kaiser
Author: Helen Mallett
Author: Ian Renfrew
Author: David Stevens
Author: Benjamin Webber

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