The CNRM Global Atmosphere Model ARPEGE‐Climat 6.3: Description and Evaluation
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- Romain Roehrig
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Isabelle Beau
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- David Saint‐Martin
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Antoinette Alias
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Bertrand Decharme
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Jean‐François Guérémy
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Aurore Voldoire
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Ahmat Younous Abdel‐Lathif
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Eric Bazile
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Sophie Belamari
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Sebastien Blein
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Dominique Bouniol
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Yves Bouteloup
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Julien Cattiaux
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Fabrice Chauvin
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Matthieu Chevallier
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Jeanne Colin
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Hervé Douville
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Pascal Marquet
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Martine Michou
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Pierre Nabat
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Thomas Oudar
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Philippe Peyrillé
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Jean‐Marcel Piriou
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- David Salas y Mélia
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Roland Séférian
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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- Stéphane Sénési
- CNRM, Université de Toulouse, Météo‐France, CNRS Toulouse France
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説明
<jats:title>Abstract</jats:title><jats:p>The present study describes the atmospheric component of the sixth‐generation climate models of the Centre National de Recherches Météorologiques (CNRM), namely, ARPEGE‐Climat 6.3. It builds up on more than a decade of model development and tuning efforts, which led to major updates of its moist physics. The vertical resolution has also been significantly increased, both in the boundary layer and in the stratosphere. ARPEGE‐Climat 6.3 is now coupled to the new version (8.0) of the SURFace EXternalisée (SURFEX) surface model, in which several new features (e.g., floodplains, aquifers, and snow processes) improve the water cycle realism. The model calibration is discussed in depth. An <jats:italic>amip</jats:italic>‐type experiment, in which the sea surface temperatures and sea ice concentrations are prescribed, and following the CMIP6 protocol, is extensively evaluated, in terms of climate mean state and variability. ARPEGE‐Climat 6.3 is shown to improve over its previous version (5.1) by many climate features. Major improvements include the top‐of‐atmosphere and surface energy budgets in their various components (shortwave and longwave, total and clear sky), cloud cover, near‐surface temperature, precipitation climatology and daily‐mean distribution, and water discharges at the outlet of major rivers. In contrast, clouds over subtropical stratocumulus decks, several dynamical variables (sea level pressure, 500‐hPa geopotential height), are still significantly biased. The tropical intraseasonal variability and diurnal cycle of precipitation, though improved, remained area of concerns for further model improvement. New biases also emerge, such as a lack of precipitation over several tropical continental areas. Within the CMIP6 context, ARPEGE‐Climat 6.3 is the atmospheric component of CNRM‐CM6‐1 and CNRM‐ESM2‐1.</jats:p>
収録刊行物
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- Journal of Advances in Modeling Earth Systems
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Journal of Advances in Modeling Earth Systems 12 (7), 2020-07
American Geophysical Union (AGU)