The higher-dimensional -equation is a family of PDEs, introduced by Holm and Staley (2003), that describe the motion of shallow water waves in -dimensions. It expresses the invariance of the Lie-transport of the momentum one-form density associated with the fluid in -dimensions. The constant can also be viewed as a balance parameter between fluid convection and fluid stretching/expansion. In this article, we interpret this family of PDEs as the geodesic equation of a right-invariant affine connection on the diffeomorphism group of . Using this framework and the methods of Ebin and Marsden (1970), we show local well-posedness of the -equation with a Fourier multiplier as the inertia operator. This is achieved by formulating the -equation as a smooth ODE on a Hilbert manifold, applying Picard-Lindelöf, and transferring back to the smooth category by showing that there is no loss of spatial regularity during the time evolution.

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