Articles | Volume 8, issue 4
https://doi.org/10.5194/tc-8-1361-2014
https://doi.org/10.5194/tc-8-1361-2014
Research article
 | 
31 Jul 2014
Research article |  | 31 Jul 2014

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

H. Fréville, E. Brun, G. Picard, N. Tatarinova, L. Arnaud, C. Lanconelli, C. Reijmer, and M. van den Broeke

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Cited articles

Anderson, P. S. and Neff, W. D.: Boundary layer physics over snow and ice, Atmos. Chem. Phys., 8, 3563–3582, https://doi.org/10.5194/acp-8-3563-2008, 2008.
Balsamo, G., Beljaars, A., Scipal, K., Viterbo, P., van den Hurk, B., Hirschi, M., and Betts, A. K.: A revised hydrology for the ECMWF model: Verification from field site to terrestrial water storage and impact in the Integrated Forecast System, J. Hydrometeorol., 10, 623–643, 2009.
Balsamo, G., Albergel, C., Beljaars, A., Boussetta, S., Brun, E., Cloke, H., Dee, D., Dutra, E., Pappenberger, F., de Rosnay, P., Muñoz-Sabater, J., Stockdale, T., and Vitart, F.: ERA-Interim/Land: A global land-surface reanalysis based on ERA-Interim meteorological forcing, ERA Report Series, ECMWF, Shinfield Park, Reading, 2012.
Bamber, J. and Gomez-Dans, J. L.: The accuracy of digital elevation models of the Antarctic continent, Earth Planet. Sc. Lett., 237, 516–523, 2005.
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