Titlebook: Nonlinear Water Waves; IUTAM Symposium, Tok Kiyoshi Horikawa,Hajime Maruo Conference proceedings 1988 Springer-Verlag, Berlin, Heidelberg 1

Jefferson

书目名称Nonlinear Water Waves影响因子(影响力)




书目名称Nonlinear Water Waves影响因子(影响力)学科排名




书目名称Nonlinear Water Waves网络公开度




书目名称Nonlinear Water Waves网络公开度学科排名




书目名称Nonlinear Water Waves被引频次




书目名称Nonlinear Water Waves被引频次学科排名




书目名称Nonlinear Water Waves年度引用




书目名称Nonlinear Water Waves年度引用学科排名




书目名称Nonlinear Water Waves读者反馈




书目名称Nonlinear Water Waves读者反馈学科排名

可互换

Recent Developments in the Modelling of Unsteady and Breaking Water Wavesuation for irrotational flow was used together with time marching of the position and velocity potential of surface particles using the free surface boundary conditions. Most subsequent work uses boundary integral formulations. Marker and cell (MAC) methods have also been used to a lesser extent; ho

门闩

人类

变量

On the Initial Evolution of Gravity-Capillary Wavese SAR, that can provide information about surface waves with a wavelength of the order of 4–40 cm, i.e. in the gravity-capillary range. It was thus found that in shallow waters these waves experience a strong modulation in the presence of a non-uniform current and a varying bottom topography. (see e

Prognosis

Nonlinear Forced Water Waves in a Shallow Channel near a Cut-off Frequencychannel near a cut-off frequency. It is shown, through a perturbation analysis using characteristic variables, that the nonlinear response is governed by a forced Kadomtsev-Petviashvili (KP) equation with periodic boundary conditions across the channel; this nonlinear initial-boundary-value problem

osculate

Ossification

Asymptotic Behavior of a Shallow-Water Soliton Reflected at a Sloping Beachhown that the boundary-value problem for the Boussinesq equation under the “reduced” boundary condition is simplified to an “initial value” problem for the Korteweg-de Vries equation in the form of the spatial evolution of the reflected wave. Solving it numerically, the asymptotic behavior is demons

Dorsal-Kyphosis

Normal Form and Solitons in the Shallow Water Wavesnsion. The KdV equation admits a family of solitary waves called solitons having the remarkable property that the result of interaction of solitons leaves their shape unaltered, except a phase shift. This elastic interaction is due to the fact that the KdV equation possesses an infinite number of co

orthopedist