Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea

Coastal polynyas are areas in an ice-covered ocean where the ice cover is exported, mostly by off-shore winds. The resulting reduction of sea ice enables an enhanced ocean-atmosphere heat transfer. Once the water temperatures are at the freezing point, further heat loss induces sea ice production. T...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Haid, Verena, Timmermann, Ralph
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2013
Subjects:
Online Access:https://epic.awi.de/id/eprint/32474/
http://onlinelibrary.wiley.com/doi/10.1002/jgrc.20133/abstract
https://hdl.handle.net/10013/epic.41922
id ftawi:oai:epic.awi.de:32474
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spelling ftawi:oai:epic.awi.de:32474 2024-09-15T17:47:06+00:00 Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea Haid, Verena Timmermann, Ralph 2013-05-30 https://epic.awi.de/id/eprint/32474/ http://onlinelibrary.wiley.com/doi/10.1002/jgrc.20133/abstract https://hdl.handle.net/10013/epic.41922 unknown American Geophysical Union Haid, V. and Timmermann, R. (2013) Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea , JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, 118 , pp. 2640-2652 . doi:10.1002/jgrc.20133 <https://doi.org/10.1002/jgrc.20133> , hdl:10013/epic.41922 EPIC3JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, American Geophysical Union, 118, pp. 2640-2652 Article isiRev 2013 ftawi https://doi.org/10.1002/jgrc.20133 2024-06-24T04:06:16Z Coastal polynyas are areas in an ice-covered ocean where the ice cover is exported, mostly by off-shore winds. The resulting reduction of sea ice enables an enhanced ocean-atmosphere heat transfer. Once the water temperatures are at the freezing point, further heat loss induces sea ice production. The heat exchange and ice production in coastal polynyas in the southwestern Weddell Sea is addressed using the Finite-Element Sea-ice Ocean Model, a primitive-equation, hydrostatic ocean circulation model coupled with a dynamic-thermodynamic sea-ice model, which allows to quantify the amount of heat associated with cooling of the water column. Three important polynya regions are identified: at Brunt Ice Shelf, at Ronne Ice Shelf and along the southern part of the Antarctic Peninsula. Multiyear winter means (May–September 1990–2009) give an upward heat flux to the atmosphere of 311 W/m^2 in the Brunt polynyas, 511 W/m^2 in Ronne Polynya and 364 W/m^2 in the Antarctic Peninsula polynyas, whereof 57 W/m^2, 49 W/m^2 and 48 W/m^2, respectively, are supplied as oceanic heat flux from deeper layers. The mean winter sea ice production is 7.2 cm/d in the Brunt polynyas corresponding to an ice volume of 1.3x10^10 m^3/winter, 13.2 cm/d at Ronne polynya (4.4x10^10 m^3/winter), and 9.2 cm/d in the Antarctic Peninsula polynyas (2.1x10^10 m^3/winter). The heat flux to the atmosphere inside polynyas is 7 to 9 times higher than the heat flux in the adjacent area; polynya ice production per unit area exceeds adjacent values by a factor of 9 to 14. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Brunt Ice Shelf Ice Shelf Ronne Ice Shelf Sea ice Weddell Sea Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Journal of Geophysical Research: Oceans 118 5 2640 2652
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Coastal polynyas are areas in an ice-covered ocean where the ice cover is exported, mostly by off-shore winds. The resulting reduction of sea ice enables an enhanced ocean-atmosphere heat transfer. Once the water temperatures are at the freezing point, further heat loss induces sea ice production. The heat exchange and ice production in coastal polynyas in the southwestern Weddell Sea is addressed using the Finite-Element Sea-ice Ocean Model, a primitive-equation, hydrostatic ocean circulation model coupled with a dynamic-thermodynamic sea-ice model, which allows to quantify the amount of heat associated with cooling of the water column. Three important polynya regions are identified: at Brunt Ice Shelf, at Ronne Ice Shelf and along the southern part of the Antarctic Peninsula. Multiyear winter means (May–September 1990–2009) give an upward heat flux to the atmosphere of 311 W/m^2 in the Brunt polynyas, 511 W/m^2 in Ronne Polynya and 364 W/m^2 in the Antarctic Peninsula polynyas, whereof 57 W/m^2, 49 W/m^2 and 48 W/m^2, respectively, are supplied as oceanic heat flux from deeper layers. The mean winter sea ice production is 7.2 cm/d in the Brunt polynyas corresponding to an ice volume of 1.3x10^10 m^3/winter, 13.2 cm/d at Ronne polynya (4.4x10^10 m^3/winter), and 9.2 cm/d in the Antarctic Peninsula polynyas (2.1x10^10 m^3/winter). The heat flux to the atmosphere inside polynyas is 7 to 9 times higher than the heat flux in the adjacent area; polynya ice production per unit area exceeds adjacent values by a factor of 9 to 14.
format Article in Journal/Newspaper
author Haid, Verena
Timmermann, Ralph
spellingShingle Haid, Verena
Timmermann, Ralph
Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea
author_facet Haid, Verena
Timmermann, Ralph
author_sort Haid, Verena
title Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea
title_short Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea
title_full Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea
title_fullStr Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea
title_full_unstemmed Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea
title_sort simulated heat flux and sea ice production at coastal polynyas in the southwestern weddell sea
publisher American Geophysical Union
publishDate 2013
url https://epic.awi.de/id/eprint/32474/
http://onlinelibrary.wiley.com/doi/10.1002/jgrc.20133/abstract
https://hdl.handle.net/10013/epic.41922
genre Antarc*
Antarctic
Antarctic Peninsula
Brunt Ice Shelf
Ice Shelf
Ronne Ice Shelf
Sea ice
Weddell Sea
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Brunt Ice Shelf
Ice Shelf
Ronne Ice Shelf
Sea ice
Weddell Sea
op_source EPIC3JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, American Geophysical Union, 118, pp. 2640-2652
op_relation Haid, V. and Timmermann, R. (2013) Simulated heat flux and sea ice production at coastal polynyas in the southwestern Weddell Sea , JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, 118 , pp. 2640-2652 . doi:10.1002/jgrc.20133 <https://doi.org/10.1002/jgrc.20133> , hdl:10013/epic.41922
op_doi https://doi.org/10.1002/jgrc.20133
container_title Journal of Geophysical Research: Oceans
container_volume 118
container_issue 5
container_start_page 2640
op_container_end_page 2652
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