Transversally periodic solitary gravity-capillary waves

被引:16
作者
Milewski, Paul A. [1 ]
Wang, Zhan [2 ]
机构
[1] Univ Bath, Dept Math Sci, Bath BA2 7AY, Avon, England
[2] UCL, Dept Math, London WC1E 6BT, England
来源
PROCEEDINGS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES | 2014年 / 470卷 / 2161期
基金
英国工程与自然科学研究理事会;
关键词
gravity-capillary; solitary wave; periodic wave; breather; FREE-SURFACE FLOWS; WATER-WAVES; DEEP-WATER; EQUATION; MODEL; INSTABILITY; STABILITY; DYNAMICS; WIND;
D O I
10.1098/rspa.2013.0537
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
When both gravity and surface tension effects are present, surface solitary water waves are known to exist in both two- and three-dimensional infinitely deep fluids. We describe here solutions bridging these two cases: travelling waves which are localized in the propagation direction and periodic in the transverse direction. These transversally periodic gravity-capillary solitary waves are found to be of either elevation or depression type, tend to plane waves below a critical transverse period and tend to solitary lumps as the transverse period tends to infinity. The waves are found numerically in a Hamiltonian system for water waves simplified by a cubic truncation of the Dirichlet-to-Neumann operator. This approximation has been proved to be very accurate for both two- and three-dimensional computations of fully localized gravity-capillary solitary waves. The stability properties of these waves are then investigated via the time evolution of perturbed wave profiles.
引用
收藏
页数:17
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