Local well-posedness of the higher-dimensional $b$-equation
Justin Valletta
TL;DR
The paper addresses local well-posedness for the $n$-dimensional $b$-equation by casting it as the geodesic flow of a right-invariant affine connection on the diffeomorphism group, using a Fourier multiplier inertia operator. The authors extend the Ebin–Marsden no-loss no-gain framework to a non-metric, affine-connection setting, proving a smooth geodesic spray on the Hilbert manifold $T ext{D}^s(R^n)$ and obtaining local existence and uniqueness via Picard–Lindelöf for $s>n/2+1$ with $s\ge r$ and inertia operator class $oxed{ ext{E}^r}$ ($r\ge 1$). They also establish a Kelvin-Noether circulation theorem and show no loss of spatial regularity, allowing the $H^s$-well-posedness to lift to the smooth category, yielding local well-posedness in $H^ty(R^n,R^n)$. The results rigorously connect multi-dimensional shallow-water models to geometric hydrodynamics and provide a solid analytical foundation for the higher-dimensional $b$-equation with general inertia operators. This advances understanding of well-posedness for non-metric Euler-Arnold flows and their associated conservation structures in fluid dynamics.
Abstract
The higher-dimensional $b$-equation is a family of PDEs, introduced by Holm and Staley (2003), that describe the motion of shallow water waves in $n$-dimensions. It expresses the invariance of the Lie-transport of the momentum one-form density associated with the fluid in $b$-dimensions. The constant $b$ 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 $\mathbb{R}^n$. Using this framework and the methods of Ebin and Marsden (1970), we show local well-posedness of the $b$-equation with a Fourier multiplier as the inertia operator. This is achieved by formulating the $b$-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.
