Global existence for small amplitude semilinear wave equations with time-dependent scale-invariant damping
Daoyin He, Yaqing Sun, Kangqun Zhang
TL;DR
The paper proves sharp global existence for small data in semilinear wave equations with time-dependent, scale-invariant damping by transforming to a semilinear generalized Tricomi equation and establishing new weighted Strichartz estimates. The core strategy combines a time-change and angular-FIO analysis to derive endpoint and inhomogeneous bounds, followed by a Picard iteration to obtain global weak solutions for exponents in the range $p_{\text{crit}}(n,\mu)<p\le p_{\text{conf}}(n,\mu)$ with $n\ge3$ and $\mu\in(0,1)\cup(1,2)$. The work develops a comprehensive toolkit of weighted estimates for the generalized Tricomi operator, including dyadic decompositions, stationary-phase arguments, and complex interpolation to handle delicate endpoint cases. It also discusses the limiting cases $\mu=1$ and the $n=2$ setting, outlining open questions and related results. The results advance understanding of damping-driven global behavior in nonlinear waves and provide a framework for further refinements in low dimensions and borderline damping regimes.
Abstract
In this paper we prove a sharp global existence result for semilinear wave equations with time-dependent scale-invariant damping terms if the initial data is small. More specifically, we consider Cauchy problem of $\partial_t^2u-Δu+\fracμ{t}\partial_tu=|u|^p$, where $n\ge 3$, $t\ge 1$ and $μ\in(0,1)\cup(1,2)$. For critical exponent $p_{crit}(n,μ)$ which is the positive root of $(n+μ-1)p^2-(n+μ+1)p-2=0$ and conformal exponent $p_{conf}(n,μ)=\frac{n+μ+3}{n+μ-1}$, we establish global existence for $n\geq3$ and $p_{crit}(n,μ)<p\leq p_{conf}(n,μ)$. The proof is based on changing the wave equation into the semilinear generalized Tricomi equation $\partial_t^2u-t^mΔu=t^{α(m)}|u|^p$, where $m=m(μ)>0$ and $α(m)\in\Bbb R$ are two suitable constants, then we investigate more general semilinear Tricomi equation $\partial_t^2v-t^mΔv=t^α|v|^p$ and establish related weighted Strichartz estimates. Returning to the original wave equation, the corresponding global existence results on the small data solution $u$ can be obtained.
