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In geophysical fluid dynamics, the f-plane … In geophysical fluid dynamics, the f-plane approximation is an approximation where the Coriolis parameter, denoted f, is set to a constant value. This approximation is frequently used for the analysis of highly idealized tropical cyclones. Using a constant Coriolis parameter prevents the formation of which are largely responsible for the North-westward direction of most tropical cyclones. Rossby waves also depend on variations in f, and do not occur in the f-plane approximation. In reality, the Coriolis parameter varies with latitude, and so the f-plane approximation is not appropriate when considering flows over large length scales. The f-plane approximation is also poor near the equator, where variations in f are on the same order of magnitude as f. The beta plane approximation is an improvement on the f-plane approximation which takes leading-order variations in f into account.eading-order variations in f into account.
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http://www.gfdl.noaa.gov/blog/isaac-held/2013/12/31/43-rotating-radiative-convective-equilibrium/ +
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| rdfs:comment |
In geophysical fluid dynamics, the f-plane … In geophysical fluid dynamics, the f-plane approximation is an approximation where the Coriolis parameter, denoted f, is set to a constant value. This approximation is frequently used for the analysis of highly idealized tropical cyclones. Using a constant Coriolis parameter prevents the formation of which are largely responsible for the North-westward direction of most tropical cyclones. Rossby waves also depend on variations in f, and do not occur in the f-plane approximation.do not occur in the f-plane approximation.
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| rdfs:label |
F-plane
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