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Title: Impacts of a mushy-layer thermodynamic approach in global sea-ice simulations using the CICE sea-ice model

Authors:
 [1];  [1]
  1. T-3 Fluid Dynamics and Solid Mechanics Group, Theoretical Division, Los Alamos National Laboratory, Los Alamos New Mexico USA
Publication Date:
Sponsoring Org.:
USDOE National Nuclear Security Administration (NNSA)
OSTI Identifier:
1402292
Grant/Contract Number:
AC52-06NA25396
Resource Type:
Journal Article: Publisher's Accepted Manuscript
Journal Name:
Journal of Geophysical Research. Oceans
Additional Journal Information:
Journal Volume: 120; Journal Issue: 2; Related Information: CHORUS Timestamp: 2017-10-23 17:53:10; Journal ID: ISSN 2169-9275
Publisher:
Wiley Blackwell (John Wiley & Sons)
Country of Publication:
United States
Language:
English

Citation Formats

Turner, Adrian K., and Hunke, Elizabeth C.. Impacts of a mushy-layer thermodynamic approach in global sea-ice simulations using the CICE sea-ice model. United States: N. p., 2015. Web. doi:10.1002/2014JC010358.
Turner, Adrian K., & Hunke, Elizabeth C.. Impacts of a mushy-layer thermodynamic approach in global sea-ice simulations using the CICE sea-ice model. United States. doi:10.1002/2014JC010358.
Turner, Adrian K., and Hunke, Elizabeth C.. Wed . "Impacts of a mushy-layer thermodynamic approach in global sea-ice simulations using the CICE sea-ice model". United States. doi:10.1002/2014JC010358.
@article{osti_1402292,
title = {Impacts of a mushy-layer thermodynamic approach in global sea-ice simulations using the CICE sea-ice model},
author = {Turner, Adrian K. and Hunke, Elizabeth C.},
abstractNote = {},
doi = {10.1002/2014JC010358},
journal = {Journal of Geophysical Research. Oceans},
number = 2,
volume = 120,
place = {United States},
year = {Wed Feb 25 00:00:00 EST 2015},
month = {Wed Feb 25 00:00:00 EST 2015}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record at 10.1002/2014JC010358

Citation Metrics:
Cited by: 7works
Citation information provided by
Web of Science

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  • The new sea ice configuration GSI6.0, used in the Met Office global coupled configuration GC2.0, is described and the sea ice extent, thickness and volume are compared with the previous configuration and with observationally based data sets. In the Arctic, the sea ice is thicker in all seasons than in the previous configuration, and there is now better agreement of the modelled concentration and extent with the HadISST data set. As a result, in the Antarctic, a warm bias in the ocean model has been exacerbated at the higher resolution of GC2.0, leading to a large reduction in ice extentmore » and volume; further work is required to rectify this in future configurations.« less
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