Relaxation to Intermediate Attractors in Nonlinear Wave Equations
Teoretičeskaâ i matematičeskaâ fizika, Tome 127 (2001) no. 3, pp. 475-487

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We study the dynamics of nonlinear wave equations near the threshold of singularity formation, motivated by some unexpected features observed in the critical gravitational collapse. One of the features, the existence of a universal intermediate attractor in the dynamics at the threshold of singularity formation, is studied in more detail. The result is a scheme of the evolution: for all initial data sufficiently near the threshold, the solutions reach one universal static solution, which plays the role of an intermediate attractor. The solutions remain near the attractor for some time, which scales in a simple way with a parameter of the initial data, and then departs in one of two “opposite” directions, eventually forming a singularity or dispersing. The relaxation as well as the departure from the attractor is governed in the linear approximation by quasi-normal modes (QNMs) and one growing mode. Moreover, the profiles of the perturbation modes with their oscillation frequencies and damping or amplifying factors, calculated as eigenvalue problems (linear ODEs) have been observed in numerical evolution (nonlinear PDEs). In particular, the exponent of the growing mode determines the lifetime of the intermediate dynamics (near the attractor), and a few least damped QNMs have been observed as ringing in the relaxation process.
@article{TMF_2001_127_3_a13,
     author = {N. Szpak},
     title = {Relaxation to {Intermediate} {Attractors} in {Nonlinear} {Wave} {Equations}},
     journal = {Teoreti\v{c}eska\^a i matemati\v{c}eska\^a fizika},
     pages = {475--487},
     publisher = {mathdoc},
     volume = {127},
     number = {3},
     year = {2001},
     language = {ru},
     url = {http://geodesic.mathdoc.fr/item/TMF_2001_127_3_a13/}
}
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N. Szpak. Relaxation to Intermediate Attractors in Nonlinear Wave Equations. Teoretičeskaâ i matematičeskaâ fizika, Tome 127 (2001) no. 3, pp. 475-487. http://geodesic.mathdoc.fr/item/TMF_2001_127_3_a13/