Publication | Open Access
Development of a Second-Generation Regional Climate Model (RegCM2). Part I: Boundary-Layer and Radiative Transfer Processes
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1993
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EngineeringClimate ModelingAtmospheric ModelEarth System ScienceEarth ScienceRegional Climate ResponseNumerical Weather PredictionRadiative TransferAtmospheric ScienceClimate ProjectionAtmospheric ModelingClimate ChangeMeteorologyGeographyClimate SystemClimatologyRadiative Transfer FormulationClimate ModellingBoundary Condition Assimilation
RegCM2, a second‑generation regional climate model, was completed at NCAR, with convective processes and boundary‑condition assimilation detailed in a companion paper. This paper evaluates month‑long European simulations to test RegCM2’s new boundary‑layer parameterization. RegCM2, built on the MM4 framework, incorporates improved boundary‑layer, radiative transfer, surface physics, cumulus convection, and time‑integration schemes, including Holtsag et al.’s boundary‑layer parameterization and the CCM2 radiative transfer package. The new schemes markedly improve precipitation, temperature, moisture, and cloudiness climatology while leaving synoptic‑pattern performance largely unchanged.
During the last few years the development of a second-generation regional climate modeling system (RegCM2) has been completed at the National Center for Atmospheric Research (NCAR). Based upon the National Center for Atmospheric Research-Pennsylvania State University Mesoscale Model (MM4), RegCM2 includes improved formulations of boundary layer, radiative transfer, surface physics, cumulus convection, and time integration technique, which make it more physically comprehensive and more computationally efficient than the previous regional climate model version. This paper discusses a number of month-long simulations over the European region that were conducted to test the new RegCM2 boundary-layer parameterization (the scheme developed by Holtsag et al.) and radiative transfer formulation [the package developed for the NCAR Community Climate Model 2 (CCM 2)]. Both schemes significantly affect the model precipitation, temperature, moisture, and cloudiness climatology, leading to overall more realistic results, while they do not substantially modify the model performance in simulating the aggregated characteristics of synoptic patterns. Description of the convective processes and procedures of boundary condition assimilation included in RegCM2 is presented in a companion paper by Giorgi et al.