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 hh (small compared with the radius of the earth) at a polar angle θ\theta. 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)sin⁡θcos⁡θ(2/3)(\omega^2 h^2/g)\sin\theta\cos\theta. It turns out that the actual southward deflection is larger than this; it equals 4(ω2h2/g)sin⁡θcos⁡θ4(\omega^2 h^2/g)\sin\theta\cos\theta. So apparently there are other effects at work. The main task of this problem is to show how the factor of 2/32/3 turns into a factor of 44. In what follows, we will keep terms up to order ω2\omega^2 (or technically ω2R/g\omega^2 R/g) and order h/Rh/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).

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