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precipitation during the night ( Nogués-Paegle and Berbery 2000 ). This lack of improvement was especially discouraging since regional models provide a means to investigate the influence of regional features on the atmospheric circulation by means of a better characterization of topography, coastal shape, land–sea ice distribution, contrasts in soil use, etc. While there are a number of research avenues that need to be explored to determine why current regional simulations are not able to substantially
precipitation during the night ( Nogués-Paegle and Berbery 2000 ). This lack of improvement was especially discouraging since regional models provide a means to investigate the influence of regional features on the atmospheric circulation by means of a better characterization of topography, coastal shape, land–sea ice distribution, contrasts in soil use, etc. While there are a number of research avenues that need to be explored to determine why current regional simulations are not able to substantially
