Verification of the numerical forecast of the WRF model for Havana, Artemisa and Mayabeque. Study of cases
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Abstract
A verification of the numerical weather forecast obtained with the WRF model was carried out for the provinces of La Habana, Artemisa and Mayabeque. The analysis was performed for three case studies that comprise different types of synoptic scale or mesoscale phenomena that affected the study region. For the simulations, two nested domains of 12 and 4 km of spatial resolution were used, selecting for verification the 4 km, and three different combinations of convection and microphysics parameterizations were used. The data of observations from the ten meteorological stations in the region were taken as a comparison standard, corresponding to the variables to mean sea level pressure, air temperature, wind speed and relative humidity. The cell-point verification methodology was used, calculating statistics to characterize the forecasting ability with said model. The meteorological stations were grouped into three regions for the differentiated study of forecast errors. It is concluded that the best simulated variable by the model is atmospheric pressure and that wind speed is the worst simulated, with a mean relative error between 14 and 621 %. The stations located on the southern coast have, in most cases, the largest forecast errors.
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