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The SQG Equation as a Geodesic Equation

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abstract

We demonstrate that the surface quasi-geostrophic (SQG) equation given by $$\theta_t + \left<u, \nabla \theta\right>= 0,\;\;\; \theta = \nabla \times (-\Delta)^{-1/2} u,$$ is the geodesic equation on the group of volume-preserving diffeomorphisms of a Riemannian manifold $M$ in the right-invariant $\dot{H}^{-1/2}$ metric. We show by example, that the Riemannian exponential map is smooth and non-Fredholm, and that the sectional curvature at the identity is unbounded of both signs.

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nlin.PS 1

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2025 1

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CONDITIONAL 1

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Numerically modelling semidirect product geodesics

nlin.PS · 2025-05-08 · conditional · novelty 6.0

Geodesic equations on self-semidirect product groups produce strongly coupled systems where peakons form and travel together, and vorticity fields exchange energy.

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  • Numerically modelling semidirect product geodesics nlin.PS · 2025-05-08 · conditional · none · ref 53 · internal anchor

    Geodesic equations on self-semidirect product groups produce strongly coupled systems where peakons form and travel together, and vorticity fields exchange energy.