scholarly journals Integrability, existence of global solutions, and wave breaking criteria for a generalization of the Camassa–Holm equation

2020 ◽  
Vol 145 (3) ◽  
pp. 537-562
Author(s):  
Priscila Leal da Silva ◽  
Igor Leite Freire
2014 ◽  
Vol 55 (9) ◽  
pp. 093101 ◽  
Author(s):  
Panpan Zhai ◽  
Zhengguang Guo ◽  
Weiming Wang

2018 ◽  
Vol 376-377 ◽  
pp. 138-143 ◽  
Author(s):  
Dan Crisan ◽  
Darryl D. Holm
Keyword(s):  

2012 ◽  
Vol 319 (3) ◽  
pp. 731-759 ◽  
Author(s):  
Guilong Gui ◽  
Yue Liu ◽  
Peter J. Olver ◽  
Changzheng Qu
Keyword(s):  

2007 ◽  
Vol 05 (01) ◽  
pp. 1-27 ◽  
Author(s):  
ALBERTO BRESSAN ◽  
ADRIAN CONSTANTIN

This paper is devoted to the continuation of solutions to the Camassa–Holm equation after wave breaking. By introducing a new set of independent and dependent variables, the evolution problem is rewritten as a semilinear hyperbolic system in an L∞space, containing a non-local source term which is discontinuous but has bounded directional variation. For a given initial condition, the Cauchy problem has a unique solution obtained as fixed point of a contractive integral transformation. Returning to the original variables, we obtain a semigroup of global dissipative solutions, defined for every initial data [Formula: see text], and continuously depending on the initial data. The new variables resolve all singularities due to possible wave breaking and ensure that energy loss occurs only through wave breaking.


Author(s):  
Christian Rohde ◽  
Hao Tang

During the typesetting process, some misprints have been introduced in the original publication of the article.


Author(s):  
Thomas M. Bendall ◽  
Colin J. Cotter ◽  
Darryl D. Holm

A famous feature of the Camassa–Holm equation is its admission of peaked soliton solutions known as peakons. We investigate this equation under the influence of stochastic transport. Noting that peakons are weak solutions of the equation, we present a finite-element discretization for it, which we use to explore the formation of peakons. Our simulations using this discretization reveal that peakons can still form in the presence of stochastic perturbations. Peakons can emerge both through wave breaking, as the slope turns vertical, and without wave breaking as the inflection points of the velocity profile rise to reach the summit.


Sign in / Sign up

Export Citation Format

Share Document