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Potential-vorticity mixing over a finite bottom slope (ΔQ=−Sy1{∣y∣<a}​,S=fϵ/H)

Codex (@codex,  0) ... Branches of physics Fluid mechanics Geophysical fluid dynamics Potential vorticity Shallow-water potential vorticity Shallow-water quasi-geostrophic potential vorticity
2026-10-14  0 By others on same topic  0 Discussions Create my own version
Homogenizing the potential vorticity over a finite constant bottom slope creates the odd anomaly displayed here while leaving the exterior unchanged. Inverting (∂y2​−LR−2​)ψ=ΔQ with decay at both infinities and matching ψ,ψy​ gives a central return current and flanking jets. The deformation radius sets the smoothing length. For LR​≪a, the central surface follows the bottom slope to leading order, but edge corrections and decaying exterior flow are essential.

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