q 2002 American Meteorological Society On the Role of Wind-Driven Sea Ice Motion on Ocean Ventilation

Simulations with a coupled ocean–atmosphere–sea ice model are used to investigate the role of wind-driven sea ice motion on ocean ventilation. Two model experiments are analyzed in detail: one including and the other excluding wind-driven sea ice transport. Model-simulated concentrations of chlorofl...

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Main Authors: Oleg A. Saenko, Andreas Schmittner, Andrew, J. Weaver
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2001
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.541.3889
http://www.cccma.ec.gc.ca/papers/osaenko/PDF/wind_ice_ocn_2002.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.541.3889 2023-05-15T13:34:28+02:00 q 2002 American Meteorological Society On the Role of Wind-Driven Sea Ice Motion on Ocean Ventilation Oleg A. Saenko Andreas Schmittner Andrew J. Weaver The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.541.3889 http://www.cccma.ec.gc.ca/papers/osaenko/PDF/wind_ice_ocn_2002.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.541.3889 http://www.cccma.ec.gc.ca/papers/osaenko/PDF/wind_ice_ocn_2002.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.cccma.ec.gc.ca/papers/osaenko/PDF/wind_ice_ocn_2002.pdf text 2001 ftciteseerx 2016-01-08T11:04:58Z Simulations with a coupled ocean–atmosphere–sea ice model are used to investigate the role of wind-driven sea ice motion on ocean ventilation. Two model experiments are analyzed in detail: one including and the other excluding wind-driven sea ice transport. Model-simulated concentrations of chlorofluorocarbons (CFCs) are compared with observations from the Weddell Sea, the southeastern Pacific, and the North Atlantic. The authors show that the buoyancy fluxes associated with sea ice divergence control the sites and rates of deep- and intermediate-water formation in the Southern Ocean. Divergence of sea ice along the Antarctic perimeter fa-cilitates bottom-water formation in the Weddell and Ross Seas. Neglecting wind-driven sea ice transport results in unrealistic bottom-water formation in Drake Passage and too-strong convection along the Southern Ocean sea ice margin, whereas convection in the Weddell and Ross Seas is suppressed. The freshwater fluxes implicitly associated with sea ice export also determine the intensity of the gyre circulation and the rate of downwelling in the Weddell Sea. In the North Atlantic, the increased sea ice export from the Arctic weakens and shallows the meridional overturning cell. This results in a decreased surface flux of CFCs around 658N by about a factor of 2. At steady state, convection in the North Atlantic is found to be less affected by the buoyancy fluxes associated with sea ice divergence when compared with that in the Southern Ocean. 1. Text Antarc* Antarctic Arctic Drake Passage North Atlantic Sea ice Southern Ocean Weddell Sea Unknown Antarctic Arctic Drake Passage Pacific Southern Ocean The Antarctic Weddell Weddell Sea
institution Open Polar
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language English
description Simulations with a coupled ocean–atmosphere–sea ice model are used to investigate the role of wind-driven sea ice motion on ocean ventilation. Two model experiments are analyzed in detail: one including and the other excluding wind-driven sea ice transport. Model-simulated concentrations of chlorofluorocarbons (CFCs) are compared with observations from the Weddell Sea, the southeastern Pacific, and the North Atlantic. The authors show that the buoyancy fluxes associated with sea ice divergence control the sites and rates of deep- and intermediate-water formation in the Southern Ocean. Divergence of sea ice along the Antarctic perimeter fa-cilitates bottom-water formation in the Weddell and Ross Seas. Neglecting wind-driven sea ice transport results in unrealistic bottom-water formation in Drake Passage and too-strong convection along the Southern Ocean sea ice margin, whereas convection in the Weddell and Ross Seas is suppressed. The freshwater fluxes implicitly associated with sea ice export also determine the intensity of the gyre circulation and the rate of downwelling in the Weddell Sea. In the North Atlantic, the increased sea ice export from the Arctic weakens and shallows the meridional overturning cell. This results in a decreased surface flux of CFCs around 658N by about a factor of 2. At steady state, convection in the North Atlantic is found to be less affected by the buoyancy fluxes associated with sea ice divergence when compared with that in the Southern Ocean. 1.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Oleg A. Saenko
Andreas Schmittner
Andrew
J. Weaver
spellingShingle Oleg A. Saenko
Andreas Schmittner
Andrew
J. Weaver
q 2002 American Meteorological Society On the Role of Wind-Driven Sea Ice Motion on Ocean Ventilation
author_facet Oleg A. Saenko
Andreas Schmittner
Andrew
J. Weaver
author_sort Oleg A. Saenko
title q 2002 American Meteorological Society On the Role of Wind-Driven Sea Ice Motion on Ocean Ventilation
title_short q 2002 American Meteorological Society On the Role of Wind-Driven Sea Ice Motion on Ocean Ventilation
title_full q 2002 American Meteorological Society On the Role of Wind-Driven Sea Ice Motion on Ocean Ventilation
title_fullStr q 2002 American Meteorological Society On the Role of Wind-Driven Sea Ice Motion on Ocean Ventilation
title_full_unstemmed q 2002 American Meteorological Society On the Role of Wind-Driven Sea Ice Motion on Ocean Ventilation
title_sort q 2002 american meteorological society on the role of wind-driven sea ice motion on ocean ventilation
publishDate 2001
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.541.3889
http://www.cccma.ec.gc.ca/papers/osaenko/PDF/wind_ice_ocn_2002.pdf
geographic Antarctic
Arctic
Drake Passage
Pacific
Southern Ocean
The Antarctic
Weddell
Weddell Sea
geographic_facet Antarctic
Arctic
Drake Passage
Pacific
Southern Ocean
The Antarctic
Weddell
Weddell Sea
genre Antarc*
Antarctic
Arctic
Drake Passage
North Atlantic
Sea ice
Southern Ocean
Weddell Sea
genre_facet Antarc*
Antarctic
Arctic
Drake Passage
North Atlantic
Sea ice
Southern Ocean
Weddell Sea
op_source http://www.cccma.ec.gc.ca/papers/osaenko/PDF/wind_ice_ocn_2002.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.541.3889
http://www.cccma.ec.gc.ca/papers/osaenko/PDF/wind_ice_ocn_2002.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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