Introduction to Classical Mechanics · Problem 10.13
Accelerating frames of reference — Morin
Physics — Mechanics · coriolis-force-deflection
Problem
Southward deflection A ball is dropped from height h (small compared with the radius of the earth) at a polar angle θ. Assume (incorrectly) that the earth is a perfect sphere. Show that a second-order Coriolis effect leads to a southward deflection (in the northern hemisphere) equal to (2/3)(ω2h2/g)sinθcosθ.
It turns out that the actual southward deflection is larger than this; it equals 4(ω2h2/g)sinθcosθ. So apparently there are other effects at work. The main task of this problem is to show how the factor of 2/3 turns into a factor of 4. In what follows, we will keep terms up to order ω2 (or technically ω2R/g) and order h/R. Also, it will be easiest to calculate southward distances relative to the point on the ground directly below the dropping point (as indicated by a plumb bob).