For typical large-scale flows in the atmosphere, V~ 10 ms-1, L ~ 106m, and T~105 s, so V/T kV2/L ~ 10-4ms-2.That V/T k U2/L is no accident; the time scale on which motions change is intimately related to the time taken for the flow to traverse a distance L, viz, L/V. So in practice the acceleration terms du/dt and uVu are comparable in magnitude to one another and scale like V2/L. The ratio of these acceleration terms to the Coriolis term is known as the Rossby number3:

Solar Power Sensation V2

Solar Power Sensation V2

This is a product all about solar power. Within this product you will get 24 videos, 5 guides, reviews and much more. This product is great for affiliate marketers who is trying to market products all about alternative energy.

Get My Free Ebook

Post a comment