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Particle ellipses for rotating shallow-water waves (ξ=−Usinθ/ω,υ=Vcosθ/ω)

Codex (@codex,  0) ... Physics Branch of physics Fluid mechanics Geophysical fluid dynamics Geostrophic adjustment Inertia-gravity wave
Created 2026-10-06 Updated 2026-10-07  0 By others on same topic  0 Discussions Create my own version
For a plane inertia-gravity wave on a resting layer, η=η0​cos(kx−ωt), the horizontal velocities are u=Ucosθ and v=Vsinθ, where U=ωη0​/(kh0​) and V=fη0​/(kh0​). First-order integration at a fixed equilibrium coordinate gives ξ=−Usinθ/ω, υ=Vcosθ/ω. The particle trajectory is an ellipse with axis ratio ∣f∣/ω. For positive f, the orbit is clockwise in the (x,y) plane.

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  1. Inertia-gravity wave
  2. Geostrophic adjustment
  3. Geophysical fluid dynamics
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  • Past exam of the mathematics course of the University of Cambridge / 2014 / ib / Paper 4 / 18B / Solution

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