Verification of a Synthesized Method for the Calculation of Low-Level Climatological Wind Fields Using a Mesoscale Boundary-Layer Model

Low-level climatological wind fields over the La Plata River region of South America are synthesized with a dry, hydrostatic mesoscale boundary-layer numerical model. The model is forced at the upper boundary with the 1200 UTC local radiosonde observations and at the lower boundary with a land-river...

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Detalles Bibliográficos
Autores principales: Berri, G.J., Nuin, J.S.G., Sraibman, L., Bertossa, G.
Formato: JOUR
Materias:
Coastal regions
Low-level wind
Synthetic climatological fields
Boundary-layer model
Climatological fields
Climatological winds
Differential heating
Diurnal cycle
Ensemble methods
Frequency distributions
High resolution
Local standard time
Lower boundary
matrix
Mean values
Mean wind speed
Mean-winds
Mesoscale
Meteorological observation
Meteorological station
Numerical models
Probability of occurrence
Root-mean square errors
Simplified method
South America
Thermal contrasts
Upper boundary
Wind directions
Wind field
Wind speed
Air pollution control
Boundary layers
Coastal zones
Errors
Meteorology
Radiosondes
Wind effects
Numerical methods
boundary layer
climate modeling
mesoscale meteorology
model validation
numerical model
observational method
wind direction
wind field
La Plata Basin
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00068314_v142_n2_p329_Berri
Aporte de:
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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