Articles | Volume 8, issue 4
The Cryosphere, 8, 1623–1623, 2014
https://doi.org/10.5194/tc-8-1623-2014
The Cryosphere, 8, 1623–1623, 2014
https://doi.org/10.5194/tc-8-1623-2014

  28 Aug 2014

28 Aug 2014

Corrigendum to "Using MODIS land surface temperatures and the Crocus snow model to understand the warm bias of ERA-Interim reanalyses at the surface in Antarctica" published in The Cryosphere, 8, 1361–1373, 2014

H. Fréville1, E. Brun1, G. Picard2,3, N. Tatarinova1, L. Arnaud2,3, C. Lanconelli4, C. Reijmer5, and M. van den Broeke5 H. Fréville et al.
  • 1CNRM-GAME UMR3589, Météo-France and CNRS, Toulouse, France
  • 2University Grenoble Alpes, LGGE UMR5183, 38041 Grenoble, France
  • 3CNRS, LGGE UMR5183, 38041 Grenoble, France
  • 4Institute of Atmospheric Sciences and Climate, Bologna, Italy
  • 5Institute for Marine and Atmospheric Research Utrecht, University of Utrecht, Utrecht, the Netherlands