The two-dimensional periodic $b$-equation on the diffeomorphism group of the torus

TL;DR

This paper explores the geometric interpretation of the two-dimensional periodic b-equation on the torus, analyzing well-posedness, curvature, and the unique role of b=2 in the geodesic flow within the diffeomorphism group.

Contribution

It provides well-posedness results, explicit curvature calculations for the 2D Camassa-Holm case, and proves the uniqueness of b=2 for weakly Riemannian geodesic flows.

Findings

b=2 is the only case with weakly Riemannian geodesic flow

Explicit curvature computations for the 2D Camassa-Holm equation

Well-posedness results for the 2D b-equation

Abstract

In this paper, the two-dimensional periodic $b$-equation is discussed under geometric aspects, i.e., as a geodesic flow on the diffeomorphism group of the torus $\T=S^1\times S^1$. In the framework of Arnold's [V.I. Arnold, Sur la g\'eom\'etrie diff\'erentielle des groupes de Lie de dimension infinie et ses applications \`a l'hydrodynamique des fluides parfaits. Ann. Inst. Fourier (Grenoble) 16 (1966) 319-361] famous approach, we achieve some well-posedness results for the $b$-equation and we perform explicit curvature computations for the 2D Camassa-Holm equation, which is obtained for $b=2$. Finally, we explain the special role of the choice $b=2$ by giving a rigorous proof that $b=2$ is the only case in which the associated geodesic flow is weakly Riemannian.