Evaluation of CMIP6 DECK Experiments With CNRM‐CM6‐1

Aurore Voldoire (1) , David Saint-Martin (1) , Stéphane Sénési (1) , B. Decharme (1) , A. Alias (1) , Matthieu Chevallier (1) , Jeanne Colin (2) , Jean-François Guérémy (1) , M. Michou (1) , Marie-Pierre Moine (3) , Pierre Nabat (1) , Romain Roehrig (1) , David Salas y Mélia (1) , Roland Séférian (1) , Sophie Valcke (3) , Isabelle Beau (1) , Sophie Belamari (1) , Sarah Berthet (1) , Christophe Cassou (3) , Julien Cattiaux (1) , Julie Deshayes (4) , Hervé Douville (1) , Christian Éthé (4) , Laurent Franchistéguy (1) , Olivier Geoffroy (1) , Claire Lévy (4) , Gurvan Madec (4) , Yann Meurdesoif (5) , Rym M'Sadek (3) , Aurélien Ribes (1) , Emilia Sanchez-Gomez (3) , Laurent Terray (3) , Robin Waldman (1)

1 GMGEC - Groupe de Météorologie de Grande Échelle et Climat
2 CNRM - Centre national de recherches météorologiques
3 CERFACS - Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique
4 NEMO R&D - Nucleus for European Modeling of the Ocean
5 LSCE - Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette]

This paper describes the main characteristics of CNRM-CM6-1, the fully coupled atmosphere-ocean general circulation model of sixth generation jointly developed by Centre National de Recherches Météorologiques (CNRM) and Cerfacs for the sixth phase of the Coupled Model Intercomparison Project 6 (CMIP6). The paper provides a description of each component of CNRM-CM6-1, including the coupling method and the new online output software. We emphasize where model's components have been updated with respect to the former model version, CNRM-CM5.1. In particular, we highlight major improvements in the representation of atmospheric and land processes. A particular attention has also been devoted to mass and energy conservation in the simulated climate system to limit long-term drifts. The climate simulated by CNRM-CM6-1 is then evaluated using CMIP6 historical and Diagnostic, Evaluation and Characterization of Klima (DECK) experiments in comparison with CMIP5 CNRM-CM5.1 equivalent experiments. Overall, the mean surface biases are of similar magnitude but with different spatial patterns. Deep ocean biases are generally reduced, whereas sea ice is too thin in the Arctic. Although the simulated climate variability remains roughly consistent with CNRM-CM5.1, its sensitivity to rising CO 2 has increased: the equilibrium climate sensitivity is 4.9 K, which is now close to the upper bound of the range estimated from CMIP5 models.

Domaines: Océan, Atmosphère

Aurore Voldoire, David Saint-Martin, Stéphane Sénési, B. Decharme, A. Alias, et al.. Evaluation of CMIP6 DECK Experiments With CNRM‐CM6‐1. Journal of Advances in Modeling Earth Systems, 2019, 11 (7), pp.2177-2213. ⟨10.1029/2019ms001683⟩. ⟨hal-02346111⟩