ﻻ يوجد ملخص باللغة العربية
In this paper, we study the number of traveling wave families near a shear flow $(u,0)$ under the influence of Coriolis force, where the traveling speeds lie outside the range of $u$. Let $beta$ be the Rossby number. If the flow $u$ has at least one critical point at which $u$ attains its minimal (resp. maximal) value, then a unique transitional $beta$ value exists in the positive (resp. negative) half-line such that the number of traveling wave families near $(u,0)$ changes suddenly from finite one to infinity when $beta$ passes through it. If $u$ has no such critical points, then the number is always finite for positive (resp. negative) $beta$ values. This is true for general shear flows under a technical assumption, and for flows in class $mathcal{K}^+$ unconditionally. The sudden change of the number of traveling wave families indicates that nonlinear dynamics around the shear flow is much richer than the non-rotating case, where no such traveling waves exist.
We consider the stability of periodic gravity free-surface water waves traveling downstream at a constant speed over a shear flow of finite depth. In case the free surface is flat, a sharp criterion of linear instability is established for a general
Let $(X,g)$ be a compact manifold with conic singularities. Taking $Delta_g$ to be the Friedrichs extension of the Laplace-Beltrami operator, we examine the singularities of the trace of the half-wave group $e^{- i t sqrt{ smash[b]{Delta_g}}}$ arisin
We study traveling wave solutions of the nonlinear variational wave equation. In particular, we show how to obtain global, bounded, weak traveling wave solutions from local, classical ones. The resulting waves consist of monotone and constant segment
We consider an epidemic model with direct transmission given by a system of nonlinear partial differential equations and study the existence of traveling wave solutions. When the basic reproductive number of the considered model is less than one, we
We describe traveling waves in a basic model for three-dimensional water-wave dynamics in the weakly nonlinear long-wave regime. Small solutions that are periodic in the direction of translation (or orthogonal to it) form an infinite-dimensional fami