| 词条 | F-plane |
| 释义 |
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 beta gyres 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 lengthscales. 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. References
See also
1 : Atmospheric dynamics |
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