Using MODIS land surface temperatures and the Crocus snow model to understand the warm bias of ERA-Interim reanalyses at the surface in Antarctica (Q61044050)

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Using MODIS land surface temperatures and the Crocus snow model to understand the warm bias of ERA-Interim reanalyses at the surface in Antarctica
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    Using MODIS land surface temperatures and the Crocus snow model to understand the warm bias of ERA-Interim reanalyses at the surface in Antarctica (English)
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    H. Fréville
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    E. Brun
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    N. Tatarinova
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    L. Arnaud
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    31 July 2014
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    8
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    1361-1373
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    4
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