研讨班报告

调和分析和偏微分方程研讨班:Transverse linear stability of one-dimensional solitary gravity water waves in a channel with finite depth

发布时间:2024-01-02
 

中科院数学与系统科学研究院

数学研究所

调和分析及其应用研究中心

学术报告

调和分析和偏微分方程研讨班


报告人孙长贞 (University of Franche-Comte)

 Transverse linear stability of one-dimensional solitary gravity water waves in a channel with finite depth

  2024.01.03(星期三)15:00-16:00

 点:思源楼S615

  要:The two dimensional gravity water wave system in a channel with finite depth admits a family of solitary waves (referred to as line solitary wave). The linear asymptotic stability of these line solitary water waves has been established by Pego and S.Sun, while the nonlinear stability remains open. Given the fact that the dispersion effect is stronger in higher dimension, it is anticipated that the nonlinear stability would be relatively easier to achieve in higher dimension. As a first step towards the nonlinear stability, we study the linear stability of line solitary waves for the three dimensional gravity water wave system—referred to as transverse linear stability.

It is found that the small amplitude line solitary waves are transversely linear stable within the exponentially weighted space. More precisely,  the semigroup of the linearized operator around the solitary waves  decays exponentially within the subspace orthogonal to the space comprising continuous resonant modes. The key element of the proof relies on the uniform resolvent estimates, which are based on the semiclassical analysis, energy estimates together with KP-II approximation of the water waves in the long wave regime.

This is a joint work with Frédéric Rousset (Orsay, France).


附件: