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DOI10.1029/2020MS002075
The CNRM Global Atmosphere Model ARPEGE-Climat 6.3: Description and Evaluation
Roehrig R.; Beau I.; Saint-Martin D.; Alias A.; Decharme B.; Guérémy J.-F.; Voldoire A.; Abdel-Lathif A.Y.; Bazile E.; Belamari S.; Blein S.; Bouniol D.; Bouteloup Y.; Cattiaux J.; Chauvin F.; Chevallier M.; Colin J.; Douville H.; Marquet P.; Michou M.; Nabat P.; Oudar T.; Peyrillé P.; Piriou J.-M.; Salas y Mélia D.; Séférian R.; Sénési S.
发表日期2020
ISSN19422466
卷号12期号:7
英文摘要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 amip-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. ©2020. The Authors.
语种英语
scopus关键词Aquifers; Atmospheric temperature; Boundary layers; Budget control; Hydrogeology; Precipitation (meteorology); Sea ice; Sea level; Surface discharges; Surface properties; Surface waters; Tropics; Atmospheric components; Geo-potential heights; Near surface temperature; Precipitation climatology; Sea ice concentration; Sea surface temperature (SST); Surface energy budget; Tropical intraseasonal variability; Climate models; atmospheric modeling; boundary layer; climate modeling; climatology; cloud cover; precipitation (climatology); sea ice; sea surface temperature; stratocumulus; stratosphere; top of atmosphere
来源期刊Journal of Advances in Modeling Earth Systems
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/156693
作者单位CNRM, Université de Toulouse, Météo-France, CNRS, Toulouse, France; United Nations World Food Programme, Rome, Italy
推荐引用方式
GB/T 7714
Roehrig R.,Beau I.,Saint-Martin D.,et al. The CNRM Global Atmosphere Model ARPEGE-Climat 6.3: Description and Evaluation[J],2020,12(7).
APA Roehrig R..,Beau I..,Saint-Martin D..,Alias A..,Decharme B..,...&Sénési S..(2020).The CNRM Global Atmosphere Model ARPEGE-Climat 6.3: Description and Evaluation.Journal of Advances in Modeling Earth Systems,12(7).
MLA Roehrig R.,et al."The CNRM Global Atmosphere Model ARPEGE-Climat 6.3: Description and Evaluation".Journal of Advances in Modeling Earth Systems 12.7(2020).
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