Articles | Volume 14, issue 8
https://doi.org/10.5194/tc-14-2715-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-2715-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Brief communication
| 
27 Aug 2020
Brief communication |
| 27 Aug 2020
| 27 Aug 2020
Brief communication: Evaluating Antarctic precipitation in ERA5 and CMIP6 against CloudSat observations
Marie-Laure Roussel
CORRESPONDING AUTHOR
Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Sorbonne Université/CNRS/École Normale Supérieure – PSL Research University/École Polytechnique – IPP, Paris, France
Florentin Lemonnier
Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Sorbonne Université/CNRS/École Normale Supérieure – PSL Research University/École Polytechnique – IPP, Paris, France
Christophe Genthon
Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Sorbonne Université/CNRS/École Normale Supérieure – PSL Research University/École Polytechnique – IPP, Paris, France
Gerhard Krinner
Institut des Géosciences de l'Environnement, CNRS, Univ. Grenoble Alpes, 38000 Grenoble, France
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Latest update: 02 Apr 2025
Short summary
The Antarctic precipitation is evaluated against space radar data in the most recent climate model intercomparison CMIP6 and reanalysis ERA5. The seasonal cycle is mostly well reproduced, but relative errors are higher in areas of complex topography, particularly in the higher-resolution models. At continental and regional scales all results are biased high, with no significant progress in the more recent models. Predicting Antarctic contribution to sea level still requires model improvements.
The Antarctic precipitation is evaluated against space radar data in the most recent climate...
