2015
DOI: 10.1007/978-3-319-12547-3_3
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A Note on the Local Well-Posedness for the Whitham Equation

Abstract: We consider the initial-value problem for the bidirectional Whitham equation, a system which combines the full two-way dispersion relation from the incompressible Euler equations with a canonical shallow-water nonlinearity. We prove local well-posedness in classical Sobolev spaces in the localised as well as the periodic case, using a square-root type transformation to symmetrise the system. The existence theory requires a non-vanishing surface elevation, indicating that the problem is ill-posed for more gener… Show more

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Cited by 31 publications
(46 citation statements)
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“…0.35. It is known from Ehrnström, Pei, Wang [14] that we are in a locally well posed situation, however, the obtained solution seems very unstable as one can see in Figure 8. This experiment was repeated with different time integrators, including the symplectic first-order Euler method described in Section 4.…”
Section: Numerical Experimentsmentioning
confidence: 83%
“…0.35. It is known from Ehrnström, Pei, Wang [14] that we are in a locally well posed situation, however, the obtained solution seems very unstable as one can see in Figure 8. This experiment was repeated with different time integrators, including the symplectic first-order Euler method described in Section 4.…”
Section: Numerical Experimentsmentioning
confidence: 83%
“…The BDW system was formally derived in [1,21] from the incompressible Euler equations to model fully dispersive shallow water waves whose propagation is allowed to be both left-and rightward, and appeared in [19,22] as a full dispersion system in the Boussinesq regime with the dispersion of the water waves system. There have been several investigations on the BDW system: local well-posedness [13,18] (in homogeneous Sobolev spaces at a positive background), a logarithmically cusped wave of greatest height [11]. There are also numerical results, investigating the validity of the BDW system as a model of waves on shallow water [4], numerical bifurcation and spectral stability [5] and the observation of dispersive shock waves [24].…”
Section: Introductionmentioning
confidence: 99%
“…Moreover, if l above is sufficiently negative then the dispersion of L is very weak, and global well-posedness of (1.1) fails in classical energy spaces. In fact, the Whitham equation as a typical representative of (1.1) is locally well-posed in Sobolev spaces H s , s > 3/2, with localized or periodic initial data [9,20], but exhibits finite-time blow-up (wave-breaking) for some sufficiently smooth initial data [7,13,23] so that global well-posedness in H s (R), s > 3/2, is not possible. This kind of break-up phenomena cannot be observed in equations with strong dispersion like KdV and BO, which are globally well-posed in H s (R) for all s ≥ 1 (see [6] and [27], respectively).…”
Section: Introductionmentioning
confidence: 99%