File:Dibujo Corrientes geostróficas.png
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Schematic of geostrophic flow. The pressure gradient force (PGF) acts from high to low pressure. The Coriolis force is directed in the direction opposite to the PGF. The resulting Geostrophic flow is a balance between the PGF and the Coriolis force.
Esquema de corrientes geostróficas. La fuerza de presión de gradiente (FPG) actúa de presión alta a baja. La fuerza de Coriolis se dirige en sentido opuesto a la FPG. La corriente geostrófica resultante es un balance entre la FPG y la de Coriolis
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editDescriptionDibujo Corrientes geostróficas.png |
Español: El archivo es la traducción y mejora de https://commons.wikimedia.org/wiki/File:Geostrophic_current.pdf hecho por Ncswart |
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Author | Fernando Archuby |
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