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https://doi.org/10.5194/tcd-9-5681-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tcd-9-5681-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

  22 Oct 2015

22 Oct 2015

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This preprint was under review for the journal TC but the revision was not accepted.

Snow on Arctic sea ice: model representation and last decade changes

K. Castro-Morales1,a, R. Ricker1, and R. Gerdes1 K. Castro-Morales et al.
  • 1Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
  • anow at: Max Planck Institute for Biogeochemistry, Jena, Germany

Abstract. Together with sea ice, Arctic snow has experienced vast changes during the last decade due to a warming climate. Thus, it is relevant to study the past and present changes of Arctic snow to understand the implications to the sea ice component, precipitation, heat and radiation budgets. In this study, we analyze the changes of snow depth between 2000 and 2013 at regional scale represented in an Arctic coupled sea ice-general circulation model. We evaluate the model performance by direct comparison of the modeled snow depths (hs_mod) to snow depths from radar measurements from the NASA Operation IceBridge (hs_OIB) during the flight campaigns completed from 2009 to 2013. Despite the description of the snow in our model is simple (i.e. single layer without explicit snow redistribution processes) as in many current sea-ice models; the latitudinal distribution of hs_mod in the western Arctic is in good agreement to observations. The hs_mod is on average 3 cm thicker than hs_OIB in latitudes > 76° N. According to the model results, the hs in 2013 decreased 21 % with respect to the multi-year mean between 2000 and 2013. This snow reduction occurred mainly in FYI dominated areas, and is in good agreement to the year-to-year loss of sea ice, also well reproduced by the model. In a simple snow mass budget, our results show that 65 % of the yearly accumulated snow is lost by sublimation and snowmelt due to the heat transfer between the snow/ice interface and the atmosphere. Although the snow layer accumulates again every year, the long-term reduction in the summer sea-ice extent ultimately affects the maximum spring accumulation of snow. The model results exhibit a last decade thinning of the snowpack that is however one order of magnitude lower than previous estimates based on radar measurements. We suggest that the later is partially due to the lack of explicit snow redistribution processes in the model, emphasizing the need to include these in current sea-ice models to improve the snow representations.

K. Castro-Morales et al.

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K. Castro-Morales et al.

K. Castro-Morales et al.

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Short summary
The snow cover on Arctic sea ice is subject to vast changes due to a warming climate. In this study, we assess last decade changes of Arctic snow depth (SD) on sea-ice simulated by an Arctic general circulation model. North of 76 N, the model SD is on average 3 cm thicker than radar SD measurements. In the last decade, the mean regional SD decreased 21 % mainly in first-year ice areas. Surface snow sublimation and melt are the dominant processes responsible of this decline.
The snow cover on Arctic sea ice is subject to vast changes due to a warming climate. In this...
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