Abstract
In order to quantify the impact of the use of different parameterization schemes on regional climate model outputs, hindcast experiments have been completed applying the Regional Climate Model version 4.3 (RegCM4.3) for the Carpathian region and its surroundings at 10-km horizontal resolution with three different cumulus convection schemes. Besides, the sensitivity of outputs for subgrid-scale processes is also studied by activating the subgrid Biosphere-Atmosphere Transfer Scheme (BATS) model within other RegCM experiments. Among the analyzed factors, RegCM is most sensitive to the applied convection scheme. The impact of closure assumption related to the used convective parameterization is secondary, while the use of subgridding has less influence on the outputs. RegCM4.3 results show improved performance over our previous model simulations but still have larger amplitude for annual precipitation cycle than the measurement-based reference data. Our validation results for temperature and precipitation suggest that for the selected region, the overall best performance is achieved when using the mixed Grell-Emanuel scheme together with Fritsch and Chappell closure.
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Notes
National Center for Atmospheric Research
International Centre for Theoretical Physics
Community Climate Model 3
Biosphere-Atmosphere Transfer Scheme
European Centre for Medium-Range Weather Forecasts Reanalysis
European Space Agency Climate Change Initiative Soil Moisture, http://www.esa-soilmoisture-cci.org
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Acknowledgments
Research leading to this paper has been supported by the following sources: the Hungarian Scientific Research Fund under grant K-83909, the AGRÁRKLIMA2 project (VKSZ_12-1-2013-0034), and the EEA Grant HU04 Adaptation to Climate Change Program (EEA-C13-10). Validation data is provided from CARPATCLIM Database, which has been compiled with the support of the European Commission in JRC in 2013.
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Pieczka, I., Pongrácz, R., Szabóné André, K. et al. Sensitivity analysis of different parameterization schemes using RegCM4.3 for the Carpathian region. Theor Appl Climatol 130, 1175–1188 (2017). https://doi.org/10.1007/s00704-016-1941-4
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DOI: https://doi.org/10.1007/s00704-016-1941-4