THESIS
2012
139 p. : ill. (chiefly col.) ; 30 cm
Abstract
To compromise the computational cost and the model resolution and accuracy of wind field
over regions with complex terrain, the diagnostic downscaling of prognostic meteorological
fields is developed and employed in recent years. This approach aims at providing a simple
and efficient algorithm to generate high resolution wind data. An EPA-approved diagnostic
model (CALMET) is being used in this study for downscaling the initial guess field
generated from the output of NCAR prognostic model (WRF). Although this method has
been widely used, especially in countries or communities where computational resources is
limited, the validity of the terrain adjustment schemes in the diagnostic model and its
sensitivity to the model’s parameterization is not well documented. This kind of
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To compromise the computational cost and the model resolution and accuracy of wind field
over regions with complex terrain, the diagnostic downscaling of prognostic meteorological
fields is developed and employed in recent years. This approach aims at providing a simple
and efficient algorithm to generate high resolution wind data. An EPA-approved diagnostic
model (CALMET) is being used in this study for downscaling the initial guess field
generated from the output of NCAR prognostic model (WRF). Although this method has
been widely used, especially in countries or communities where computational resources is
limited, the validity of the terrain adjustment schemes in the diagnostic model and its
sensitivity to the model’s parameterization is not well documented. This kind of
parameterizations is of crucial importance on the accuracy of the final wind field output
from the model, especially in regions with complex terrain like Hong Kong and PRD or
regions where observational data is not available for model evaluation. This study aims at
exploring the different terrain adjustment schemes in the CALMET model. Their
limitations is discussed and documented after numerical experiments on the sensitivity of the model to different parametric relations. Improvements on the parametric relation are
also suggested which is expected to also improve the accuracy of the model. Finally, the
structure similarity of the diagnostic and prognostic downscaled wind field is evaluated to
select a currently best model option. The downscaled wind field from this option with 100m
resolution is also compared to the observation data to access the performance and seek for
further improvements.
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