The emergence of surface-based Arctic amplification

Rises in surface and lower troposphere air temperatures through the 21st century are projected to be especially pronounced over the Arctic Ocean during the cold season. This Arctic amplification is largely driven by loss of the sea ice cover, allowing for strong heat transfers from the ocean to the...

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Published in:The Cryosphere
Other Authors: Serreze, M. (author), Barrett, A. (author), Stroeve, J. (author), Kindig, D. (author), Holland, Marika (author)
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Arctic
Arctic Ocean
Sea ice
The Cryosphere
Online Access:http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-178
https://doi.org/10.5194/tc-3-11-2009
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spelling ftncar:oai:drupal-site.org:articles_15546 2023-09-05T13:16:08+02:00 The emergence of surface-based Arctic amplification Serreze, M. (author) Barrett, A. (author) Stroeve, J. (author) Kindig, D. (author) Holland, Marika (author) 2009-02-04 application/pdf http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-178 https://doi.org/10.5194/tc-3-11-2009 en eng Copernicus Publications The Cryosphere http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-178 doi:10.5194/tc-3-11-2009 ark:/85065/d7vm4d9m Copyright Authors 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Text article 2009 ftncar https://doi.org/10.5194/tc-3-11-2009 2023-08-14T18:42:09Z Rises in surface and lower troposphere air temperatures through the 21st century are projected to be especially pronounced over the Arctic Ocean during the cold season. This Arctic amplification is largely driven by loss of the sea ice cover, allowing for strong heat transfers from the ocean to the atmosphere. Consistent with observed reductions in sea ice extent, fields from both the NCEP/NCAR and JRA-25 reanalyses point to emergence of surface-based Arctic amplification in the last decade. Article in Journal/Newspaper Arctic Arctic Ocean Sea ice The Cryosphere OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Arctic Arctic Ocean The Cryosphere 3 1 11 19
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description Rises in surface and lower troposphere air temperatures through the 21st century are projected to be especially pronounced over the Arctic Ocean during the cold season. This Arctic amplification is largely driven by loss of the sea ice cover, allowing for strong heat transfers from the ocean to the atmosphere. Consistent with observed reductions in sea ice extent, fields from both the NCEP/NCAR and JRA-25 reanalyses point to emergence of surface-based Arctic amplification in the last decade.
author2 Serreze, M. (author)
Barrett, A. (author)
Stroeve, J. (author)
Kindig, D. (author)
Holland, Marika (author)
format Article in Journal/Newspaper
title The emergence of surface-based Arctic amplification
spellingShingle The emergence of surface-based Arctic amplification
title_short The emergence of surface-based Arctic amplification
title_full The emergence of surface-based Arctic amplification
title_fullStr The emergence of surface-based Arctic amplification
title_full_unstemmed The emergence of surface-based Arctic amplification
title_sort emergence of surface-based arctic amplification
publisher Copernicus Publications
publishDate 2009
url http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-178
https://doi.org/10.5194/tc-3-11-2009
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
The Cryosphere
genre_facet Arctic
Arctic Ocean
Sea ice
The Cryosphere
op_relation The Cryosphere
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-003-178
doi:10.5194/tc-3-11-2009
ark:/85065/d7vm4d9m
op_rights Copyright Authors 2009. This work is distributed under the Creative Commons Attribution 3.0 License.
op_doi https://doi.org/10.5194/tc-3-11-2009
container_title The Cryosphere
container_volume 3
container_issue 1
container_start_page 11
op_container_end_page 19
_version_ 1776197836657917952

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