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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 7, issue 6
The Cryosphere, 7, 1887–1900, 2013
https://doi.org/10.5194/tc-7-1887-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 7, 1887–1900, 2013
https://doi.org/10.5194/tc-7-1887-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 13 Dec 2013

Research article | 13 Dec 2013

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

B. A. Blazey1,2, M. M. Holland3, and E. C. Hunke4 B. A. Blazey et al.
  • 1Center for Marine Environmental Sciences (MARUM), Universität Bremen, Bremen, Germany
  • 2Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, Colorado, USA
  • 3National Center for Atmospheric Research, Boulder, Colorado, USA
  • 4Los Alamos National Laboratory, Los Alamos, New Mexico

Abstract. 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.

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