Comparative Analysis of Surface Data of Modeled and Observed Winds (Part 1)

Descripción del Articulo

In the present work, the realism of the superficial wind simulations carried out with the model is evaluated emph Weather Research and Forecasting (WRF) is evaluated, with data obtained from the QuikSCAT (Quick Scatterometer) satellite. The meridional and zonal speeds of the wind are used as compari...

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Detalles Bibliográficos
Autores: Saavedra, Miguel, Dewite, Boris, Renauld, Lionel, Pasapera, José, Jimenez, Cesar
Formato: artículo
Fecha de Publicación:2018
Institución:Universidad Nacional Mayor de San Marcos
Repositorio:Revistas - Universidad Nacional Mayor de San Marcos
Lenguaje:español
OAI Identifier:oai:ojs.csi.unmsm:article/20236
Enlace del recurso:https://revistasinvestigacion.unmsm.edu.pe/index.php/fisica/article/view/20236
Nivel de acceso:acceso abierto
Materia:Reanalysis
atmospheric circulation
wind
stress
curl
Viento
esfuerzo
rotacional
Reanálisis
Circulación oceánica
circulación atmosférica
Descripción
Sumario:In the present work, the realism of the superficial wind simulations carried out with the model is evaluated emph Weather Research and Forecasting (WRF) is evaluated, with data obtained from the QuikSCAT (Quick Scatterometer) satellite. The meridional and zonal speeds of the wind are used as comparison parameters, as well as the stresses produced on the surface of the water. The knowledge of the configuration of the wind on the oceanic surface is important because it generates processes such as the upwelling, the spiral and the Ekman pumping. The intensity with which these processes are carried out determines the diversity and biological and shing richness of a region. The behavior of the wind is analyzed in terms of its horizontal speeds, the effort produced by these speeds, which determine the drag on a free surface and the rotational wind. Correlations greater than 0.6 are obtained in the oceanic areas, far from the coast, while for coastal regions the correlations are less than 0.4.
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