the latest Shared Socioeconomic Pathways and the Representative Concentration Pathways (SSP1-2.6, SSP2-4.5, SSP3-7.0, and SSP5-8.5) provided by the France Centre National de Recherches Météorologiques (CNRM-CM) model in the Sixth Phase of Coupled Model Intercomparison Project (CMIP6) framework...
In recent years, significant efforts have been made to upgrade physical processes in the ISBA‐CTRIP land surface system for use in fully coupled climate studies using the new CNRM‐CM6 climate model or in stand‐alone mode for global hydrological applications. Here we provide a thorough descripti...
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 ...
More recently, this land surface system has been largely upgraded to improve the representation of the land surface hydrologic and thermal processes for these large-scale hydrological applications, and also for use in the new CNRM-CM6 climate model and the new CNRM-ESM2 Earth system model (...
Here we investigate the sensitivity of contrail radiative forcing due parametric uncertainty based on the atmospheric component of the CNRM-CM6-coupled model. A perturbed parameter ensemble is generated from the sampling of twenty-two adjustable parameters involved in convect...
Evaluation of marine stratocumulus simulated by the CNRM-CM6 model using the Transpose-AMIP frameworkBrient, FlorentRoehrig, RomainVoldoire, AuroreGeophysical Research Abstracts
Overall, the diurnal SST variability is reasonably well represented in the CNRM-CM6-1 with a 1 h coupling time-step and the upper ocean model resolution of 1 m. This framework is shown to be a very valuable tool to develop and validate the boundary layer physics and the coupling interface...
Here the focus in on the recent CNRM-CM6-1 model, which shows an enhanced land surface drying in response to quadrupled atmospheric CO2 compared to its CNRM-CM5 predecessor. Atmosphere-only experiments with prescribed sea surface temperature (SST) are used to decompose the simulated RH changes ...
Evaluating Marine Stratocumulus Clouds in the CNRM-CM6-1 Model Using Short-Term Hindcastsdoi:10.1029/2018ms001461Florent BrientRomain RoehrigAurore VoldoireJohn Wiley & Sons, Ltd
CNRM-CM6PETclimate changeIPCC-AR6SSP scenariosCLIMATE-CHANGEEXTREME PRECIPITATIONBIAS CORRECTIONSOUTHERN AFRICASOIL-MOISTUREIn a warming climate, drought events are projected to increase in many regions across the world, which would have detrimental impacts on water resources for agriculture activity and ...