The emergence of nonlinear Jeans-type instabilities for quasilinear wave equations

Abstract

This article contributes a key ingredient to the longstanding open problem of understanding the fully nonlinear version of Jeans instability, as highlighted by A. Rendall [Living Rev. Relativ. 8, 6 (2005)]. We establish a family of self-increasing blowup solutions for the following class of quasilinear wave equations (a model of the Peebles' and Noh-Hwang's equations) that have not previously been studied: \[ ∂2t - ( m2 (∂t )2(1+ )2 + 4(k-m2)(1+ )) = F(t,,∂μ ) \] where F is given by \[ F(t,,∂μ ):= 23 (1+) (i) self-increasing -13 ∂t (ii) damping + 43 (∂t )21+ (iii) Riccati + (m2 (∂t )2(1+ )2 + 4(k-m2) (1+ ) ) qi ∂i (iv) convection - Kij ∂i∂j. \] The result implies the solutions can attain arbitrarily large values over time, leading to self-increasing singularities at some future endpoints of null geodesics provided the inhomogeneous perturbations of data are sufficiently small. Moreover, the solution exhibits almost blowup behavior in the long-wavelength domain. This phenomenon is referred to as the nonlinear Jeans-type instability because this wave equation is closely related to the nonlinear version of the Jeans instability problem in the Euler-Poisson and Einstein-Euler systems, which characterizes the formation of nonlinear structures in the universe. The growth rate of is significantly faster than that of the solutions to the classical linearized Jeans instability.

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