Arctic Ocean sea ice snow depth evaluation and bias sensitivity in CCSM

Sea ice cover in the Arctic Ocean is a continued focus of attention. This study investigates the impact of the snow overlying the sea ice in the Arctic Ocean. The impact of snow depth biases in the Community Climate System Model (CCSM) is shown to impact not only the sea ice, but also the overall Ar...

Full description

Bibliographic Details
Published in:The Cryosphere
Other Authors: Blazey, B. (author), Holland, Marika (author), Hunke, E. (author)
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-020-214
https://doi.org/10.5194/tc-7-1887-2013
id ftncar:oai:drupal-site.org:articles_13174
record_format openpolar
spelling ftncar:oai:drupal-site.org:articles_13174 2023-09-05T13:16:16+02:00 Arctic Ocean sea ice snow depth evaluation and bias sensitivity in CCSM Blazey, B. (author) Holland, Marika (author) Hunke, E. (author) 2013-12-13 application/pdf http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-020-214 https://doi.org/10.5194/tc-7-1887-2013 en eng Copernicus Publications The Cryosphere http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-020-214 doi:10.5194/tc-7-1887-2013 ark:/85065/d7j67hts Copyright Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License. Text article 2013 ftncar https://doi.org/10.5194/tc-7-1887-2013 2023-08-14T18:37:29Z Sea ice cover in the Arctic Ocean is a continued focus of attention. This study investigates the impact of the snow overlying the sea ice in the Arctic Ocean. The impact of snow depth biases in the Community Climate System Model (CCSM) is shown to impact not only the sea ice, but also the overall Arctic climate. Following the identification of seasonal biases produced in CCSM simulations, the thermodynamic transfer through the snow–ice column is perturbed to determine model sensitivity to these biases. This study concludes that perturbations on the order of the observed biases result in modification of the annual mean conductive flux through the snow-ice column of 0.5 W m2 relative to an unmodified simulation. The results suggest that the ice has a complex response to snow characteristics, with ice of different thicknesses producing distinct reactions. Our results indicate the importance of an accurate simulation of snow on the Arctic sea ice. Consequently, future work investigating the impact of current precipitation biases and missing snow processes, such as blowing snow, densification, and seasonal changes, is warranted. 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 7 6 1887 1900
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description Sea ice cover in the Arctic Ocean is a continued focus of attention. This study investigates the impact of the snow overlying the sea ice in the Arctic Ocean. The impact of snow depth biases in the Community Climate System Model (CCSM) is shown to impact not only the sea ice, but also the overall Arctic climate. Following the identification of seasonal biases produced in CCSM simulations, the thermodynamic transfer through the snow–ice column is perturbed to determine model sensitivity to these biases. This study concludes that perturbations on the order of the observed biases result in modification of the annual mean conductive flux through the snow-ice column of 0.5 W m2 relative to an unmodified simulation. The results suggest that the ice has a complex response to snow characteristics, with ice of different thicknesses producing distinct reactions. Our results indicate the importance of an accurate simulation of snow on the Arctic sea ice. Consequently, future work investigating the impact of current precipitation biases and missing snow processes, such as blowing snow, densification, and seasonal changes, is warranted.
author2 Blazey, B. (author)
Holland, Marika (author)
Hunke, E. (author)
format Article in Journal/Newspaper
title Arctic Ocean sea ice snow depth evaluation and bias sensitivity in CCSM
spellingShingle Arctic Ocean sea ice snow depth evaluation and bias sensitivity in CCSM
title_short Arctic Ocean sea ice snow depth evaluation and bias sensitivity in CCSM
title_full Arctic Ocean sea ice snow depth evaluation and bias sensitivity in CCSM
title_fullStr Arctic Ocean sea ice snow depth evaluation and bias sensitivity in CCSM
title_full_unstemmed Arctic Ocean sea ice snow depth evaluation and bias sensitivity in CCSM
title_sort arctic ocean sea ice snow depth evaluation and bias sensitivity in ccsm
publisher Copernicus Publications
publishDate 2013
url http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-020-214
https://doi.org/10.5194/tc-7-1887-2013
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-000-000-020-214
doi:10.5194/tc-7-1887-2013
ark:/85065/d7j67hts
op_rights Copyright Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License.
op_doi https://doi.org/10.5194/tc-7-1887-2013
container_title The Cryosphere
container_volume 7
container_issue 6
container_start_page 1887
op_container_end_page 1900
_version_ 1776197915361935360