The complex landslide flow and the method of integrable systems
Shimpei Kobayashi
TL;DR
The paper addresses how the complex landslide flow on Teichmüller-space pairs relates to an integrable-systems picture of harmonic maps into $\mathbb{H}^2$. It develops a correspondence via Labourie’s operator and CGC surfaces in $\mathbb{H}^3$, using harmonic maps, extended frames, and a spectral-parameter deformation within the loop-group framework. The main result shows that the holonomy of the complex landslide flow equals the holonomy of a family of flat connections evaluated at $\lambda = \sqrt{q}$, with the flow $q \mapsto P_q(h,h^{\star})$ holomorphic due to the holomorphic dependence of the extended frame on $\lambda$. This provides a unified, integrable-systems perspective on complex landslides and their relation to complex earthquakes, with potential applications in Teichmüller theory and CGC-surface geometry.
Abstract
We investigate a connection between the complex landslide flow, defined on a pair of Teichmüller spaces, and the integrable system approach to harmonic maps into a symmetric space. We will prove that the holonomy of the complex landslide flow can be derived from the holonomy of the family of flat connections determined by a harmonic map into the hyperbolic two-space.
