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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Preprints
https://doi.org/10.5194/tc-2019-327
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-2019-327
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

  12 Feb 2020

12 Feb 2020

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A revised version of this preprint was accepted for the journal TC and is expected to appear here in due course.

Brief communication : Evaluating Antarctic precipitation in ERA5and CMIP6 against CloudSat observations

Marie-Laure Roussel1, Florentin Lemonnier1, Christophe Genthon1, and Gerhard Krinner2 Marie-Laure Roussel et al.
  • 1Laboratoire de Météorologie Dynamique, Institut Pierre-Simon Laplace, Sorbonne Université / CNRS / École Normale Supérieure – PSL Research University / École Polytechnique – IPP, Paris, France
  • 2Institut des Géosciences de l’Environnement, CNRS, Univ. Grenoble Alpes, 38000 Grenoble, France

Abstract. CMIP5, CMIP6 and ERA5 antarctic precipitations are evaluated against CloudSat data. At continental and regional scales, ERA5 and CMIP models median are biased high, with insignificant improvement from CMIP5 to CMIP6 despite near-surface temperature improvement. However, less models yield outlying overestimation in CMIP6. AMIP configurations perform better than historical ones and, surprisingly, relative errors in areas of complex topography are higher (up to 50 %) in the 5 higher resolution models. The seasonal cycle is well reproduced by the median of the CMIP models but not by ERA5. There is limited progress from CMIP5 to CMIP6 and still room for improvement.

Marie-Laure Roussel et al.

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Marie-Laure Roussel et al.

Marie-Laure Roussel et al.

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Latest update: 04 Aug 2020
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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...
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