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A realistic simulation of snow cover and its thermal properties are important for accurate modelling of permafrost. We analyse simulated relationships between air and near-surface (20  cm) soil temperatures in

A realistic simulation of snow cover and its thermal properties are important for accurate modelling of permafrost. We analyse simulated relationships between air and near-surface (20  cm) soil temperatures in the Northern Hemisphere permafrost region during winter, with a particular focus on snow insulation effects in nine land surface models, and compare them with observations from 268 Russian stations.

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    Date Created
    • 2016-08-11
    Resource Type
  • Text
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    Identifier
    • Digital object identifier: 10.5194/tc-10-1721-2016
    • Identifier Type
      International standard serial number
      Identifier Value
      1994-0416
    • Identifier Type
      International standard serial number
      Identifier Value
      1994-0424
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    Wang, W., Rinke, A., Moore, J. C., Ji, D., Cui, X., Peng, S., . . . Sherstiukov, A. B. (2016). Evaluation of air–soil temperature relationships simulated by land surface models during winter across the permafrost region. The Cryosphere, 10(4), 1721-1737. doi:10.5194/tc-10-1721-2016

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