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being designed. b. The numerical model WRF The numerical system used for this study is the Advanced Research WRF (ARW-WRF), version 2.2 ( Skamarock et al. 2005 ; Michalakes et al. 2004 ; more information is available online at http://www.wrf-model.org ), which is a mesoscale numerical weather prediction (NWP) model for operational forecasting and atmospheric research needs. The simulations are carried out using a two-way nesting technique; two grid domains, the outer with a horizontal resolution
being designed. b. The numerical model WRF The numerical system used for this study is the Advanced Research WRF (ARW-WRF), version 2.2 ( Skamarock et al. 2005 ; Michalakes et al. 2004 ; more information is available online at http://www.wrf-model.org ), which is a mesoscale numerical weather prediction (NWP) model for operational forecasting and atmospheric research needs. The simulations are carried out using a two-way nesting technique; two grid domains, the outer with a horizontal resolution
archive of the European Centre for Medium-Range Weather Forecasts (ECMWF). However, precipitation and radiation fields were produced by carefully combining low-time-resolution observationally based data with 6-hourly model diagnostic fields from reanalyses. Convective and large-scale precipitation fields from NCEP–NCAR reanalysis were rescaled so that the total precipitation for each month agreed with the monthly gridded observed precipitation from the Global Precipitation Climatology Project (GPCP
archive of the European Centre for Medium-Range Weather Forecasts (ECMWF). However, precipitation and radiation fields were produced by carefully combining low-time-resolution observationally based data with 6-hourly model diagnostic fields from reanalyses. Convective and large-scale precipitation fields from NCEP–NCAR reanalysis were rescaled so that the total precipitation for each month agreed with the monthly gridded observed precipitation from the Global Precipitation Climatology Project (GPCP