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Davey–Stewartson equation
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Davey–Stewartson equation : ウィキペディア英語版
Davey–Stewartson equation
In fluid dynamics, the Davey–Stewartson equation (DSE) was introduced in a paper by to describe the evolution of a three-dimensional wave-packet on water of finite depth.
It is a system of partial differential equations for a complex (wave-amplitude) field u\, and a real (mean-flow) field \phi\,:
:i u_t + c_0 u_ + u_ = c_1 |u|^2 u + c_2 u \phi_x,\,
:\phi_ + c_3 \phi_ = ( |u|^2 )_x.\,
The DSE is an example of a soliton equation in 2+1 dimensions. The corresponding Lax representation for it is given in .
In 1+1 dimensions the DSE reduces to the nonlinear Schrödinger equation
:i u_t + u_ + 2k |u|^2 u =0.\,
Itself, the DSE is the particular reduction of the Zakharov–Schulman system. On the other hand, the equivalent counterpart of the DSE is the Ishimori equation.
The DSE is the result of a multiple-scale analysis of modulated nonlinear surface gravity waves, propagating over a horizontal sea bed.
==See also==

* Nonlinear systems
* Ishimori equation

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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