Small-amplitude fully localised solitary waves for the full-dispersion Kadomtsev--Petviashvili equation
Mats Ehrnstr\"om, Mark Groves

TL;DR
This paper proves the existence of fully localized solitary wave solutions for the full-dispersion KP-I equation, extending known solutions from the classical KP-I model using variational and perturbative methods.
Contribution
It demonstrates the existence of localized solitary waves for the full-dispersion KP-I equation through a novel variational and perturbative approach.
Findings
Existence of fully localized solitary waves for the full-dispersion KP-I equation.
Development of a variational principle tailored for these solutions.
Identification of a critical point via minimization on a constraint set.
Abstract
The KP-I equation \[ (u_t-2uu_x+\tfrac{1}{2}(\beta-\tfrac{1}{3})u_{xxx})_x -u_{yy}=0 \] arises as a weakly nonlinear model equation for gravity-capillary waves with strong surface tension (Bond number ). This equation admits --- as an explicit solution --- a `fully localised' or `lump' solitary wave which decays to zero in all spatial directions. Recently there has been interest in the \emph{full-dispersion KP-I equation} \[u_t + m({\mathrm D}) u_x + 2 u u_x = 0,\] where is the Fourier multiplier with symbol \[ m(k) = \left( 1 + \beta |k|^2|\right)^{\frac{1}{2}} \left( \frac{\tanh |k|}{|k|} \right)^{\frac{1}{2}} \left( 1 + \frac{2k_2^2}{k_1^2} \right)^{\frac{1}{2}}, \] which is obtained by retaining the exact dispersion relation from the water-wave problem. In this paper we show that the FDKP-I equation also has a fully localised solitary-wave solution. The…
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