On oceanic forcing of Arctic climate change

Recent dramatic climate change in the Arctic is most manifested by the reduction of multiyear sea ice pack. It has been commonly associated with anomalies of surface air temperature and atmospheric circulation, which in turn have been linked to the Arctic Oscillation (AO). A typical assessment of su...

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Bibliographic Details
Main Authors: Maslowski, W., Clement, J., Jakacki, J.
Other Authors: Oceanology
Format: Article in Journal/Newspaper
Language:unknown
Published: 2006
Subjects:
Online Access:https://hdl.handle.net/10945/43395
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spelling ftnavalpschool:oai:calhoun.nps.edu:10945/43395 2024-06-09T07:42:59+00:00 On oceanic forcing of Arctic climate change Maslowski, W. Clement, J. Jakacki, J. Oceanology 2006 application/pdf https://hdl.handle.net/10945/43395 unknown European Geosciences Union 2006, Geophysical Research Abstracts, Vol. 8, 05892, 2006, SRef-ID: 1607-7962/gra/EGU06-A-05892 https://hdl.handle.net/10945/43395 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. Article 2006 ftnavalpschool 2024-05-15T00:26:04Z Recent dramatic climate change in the Arctic is most manifested by the reduction of multiyear sea ice pack. It has been commonly associated with anomalies of surface air temperature and atmospheric circulation, which in turn have been linked to the Arctic Oscillation (AO). A typical assessment of such hypotheses is the assumption of the dominant role of external atmospheric forcing and the neglect of effects of processes internal to the Arctic Ocean. Especially the oceanic thermodynamic control of sea ice through the under-ice ablation and lateral melt along marginal ice zones tends to be overlooked. However, those ice-ocean interactions may act to de-correlate AO forcing, which helps to explain some of the timing issues between AO/atmospheric forcing and recent sea ice variability. Article in Journal/Newspaper Arctic Arctic Ocean Climate change ice pack Sea ice Naval Postgraduate School: Calhoun Arctic Arctic Ocean
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language unknown
description Recent dramatic climate change in the Arctic is most manifested by the reduction of multiyear sea ice pack. It has been commonly associated with anomalies of surface air temperature and atmospheric circulation, which in turn have been linked to the Arctic Oscillation (AO). A typical assessment of such hypotheses is the assumption of the dominant role of external atmospheric forcing and the neglect of effects of processes internal to the Arctic Ocean. Especially the oceanic thermodynamic control of sea ice through the under-ice ablation and lateral melt along marginal ice zones tends to be overlooked. However, those ice-ocean interactions may act to de-correlate AO forcing, which helps to explain some of the timing issues between AO/atmospheric forcing and recent sea ice variability.
author2 Oceanology
format Article in Journal/Newspaper
author Maslowski, W.
Clement, J.
Jakacki, J.
spellingShingle Maslowski, W.
Clement, J.
Jakacki, J.
On oceanic forcing of Arctic climate change
author_facet Maslowski, W.
Clement, J.
Jakacki, J.
author_sort Maslowski, W.
title On oceanic forcing of Arctic climate change
title_short On oceanic forcing of Arctic climate change
title_full On oceanic forcing of Arctic climate change
title_fullStr On oceanic forcing of Arctic climate change
title_full_unstemmed On oceanic forcing of Arctic climate change
title_sort on oceanic forcing of arctic climate change
publishDate 2006
url https://hdl.handle.net/10945/43395
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Climate change
ice pack
Sea ice
genre_facet Arctic
Arctic Ocean
Climate change
ice pack
Sea ice
op_relation European Geosciences Union 2006, Geophysical Research Abstracts, Vol. 8, 05892, 2006, SRef-ID: 1607-7962/gra/EGU06-A-05892
https://hdl.handle.net/10945/43395
op_rights This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
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