Dispersionless equation

Dispersionless (or quasi-classical) limits of integrable partial differential equations (PDE) arise in various problems of mathematics and physics and have been intensively studied in recent literature (see, f.i., [1]-[5]). They typically arise when considering slowly modulated long waves of an integrable dispersive PDE system.

Examples

Dispersionless KP equation

The dispersionless Kadomtsev–Petviashvili equation (dKPE) has the form

 (u_t+uu_{x})_x+u_{yy}=0,\qquad (1)

It arises from the commutation

 [L_1, L_2]=0.\qquad (2)

of the following pair of 1-parameter families of vector fields

 L_1=\partial_y+\lambda\partial_x-u_x\partial_{\lambda},\qquad (3a)
 L_2=\partial_t+(\lambda^2+u)\partial_x+(-\lambda u_x+u_y)\partial_{\lambda},\qquad (3b)

where  \lambda is a spectral parameter. The dKPE is the x-dispersionless limit of the celebrated Kadomtsev–Petviashvili equation, arising when considering long waves of that system.

The Benney moment equations

The dispersionless KP system is closely related to the Benney moment hierarchy, each of which is a dispersionless integrable system:

 A^n_{t_2} + A^{n+1}_x + n A^{n-1} A^0_x =0.

These arise as the consistency condition between

 \lambda = p + \sum_{n=0}^\infty A^n/p^{n+1},

and the simplest two evolutions in the hierarchy are:

 p_{t_2} + p p_x + A^0_x =0,
 p_{t_3}  + p^2 p_x + (p A^0+A^1)_x = 0,

The dKP is recovered on setting

 u = A^0,

and eliminating the other moments, as well as identifying y=t_2 and t= t_3.

If one sets A^n = h v^n, so that the countably many moments A^n are expressed in terms of just two functions, the classical shallow water equations result:

h_y + (hv)_x=0,
v_y +v v_x + h_x=0.

These may also be derived from considering slowly modulated wave train solutions of the nonlinear Schrodinger equation. Such 'reductions', expressing the moments in terms of finitely many dependent variables, are described by the Gibbons-Tsarev equation.

Dispersionless Korteweg–de Vries equation

The dispersionless Korteweg–de Vries equation (dKdVE) reads as

 u_{t_3}=uu_{x}.\qquad (4)

It is the dispersionless or quasiclassical limit of the Korteweg–de Vries equation. It is satisfied by t_2-independent solutions of the dKP system. It is also obtainable from the t_3-flow of the Benney hierarchy on setting

 \lambda^2 = p^2 + 2A^0.

Dispersionless Novikov–Veselov equation

The dispersionless Novikov-Veselov equation is most commonly written as the following equation for a real-valued function v=v(x_1,x_2,t):


\begin{align}
& \partial_{ t } v = \partial_{ z }( v w ) + \partial_{ \bar z }( v \bar w ), \\
& \partial_{ \bar z } w = - 3 \partial_{ z } v,
\end{align}

where the following standard notation of complex analysis is used:  \partial_{ z } = \frac{ 1 }{ 2 } ( \partial_{ x_1 } - i \partial_{ x_2 } ) ,  \partial_{ \bar z } = \frac{ 1 }{ 2 } ( \partial_{ x_1 } + i \partial_{ x_2 } ) . The function w here is an auxiliary function, defined uniquely from v up to a holomorphic summand.

See also

References

External links

This article is issued from Wikipedia - version of the Tuesday, March 01, 2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.