2022
DOI: 10.48550/arxiv.2201.03628
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Long-time existence for a Whitham--Boussinesq system in two dimensions

Abstract: This paper is concerned with a two dimensional Whitham-Boussinesq system modeling surface waves of an inviscid incompressible fluid layer. We prove that the associated Cauchy problem is well-posed for initial data of low regularity, with existence time of scale O 1/ √ ǫ , where ǫ > 0 is a shallowness parameter measuring the ratio of the amplitude of the wave to the mean depth of the fluid. The key ingredients in the proof are frequency loacalised dispersive and Strichartz estimates that depend on ǫ as well as … Show more

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Cited by 2 publications
(2 citation statements)
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“…The estimates derived in the aforementioned papers are not uniform in μ. However, a recent study by Tesfahun [49] proved that the corresponding two-dimensional system (1.10) without surface tension is well-posed on a time interval of order O( 1 √ ε ) in the KdV-regime. Indeed, dispersive techniques are tailored-made for short waves and therefore seem not to be well suited to capture the long wave regime (see for instance [35] for similar results for the Boussinesq system in the KdV-KdV case).…”
Section: Former Well-posedness Resultsmentioning
confidence: 99%
“…The estimates derived in the aforementioned papers are not uniform in μ. However, a recent study by Tesfahun [49] proved that the corresponding two-dimensional system (1.10) without surface tension is well-posed on a time interval of order O( 1 √ ε ) in the KdV-regime. Indeed, dispersive techniques are tailored-made for short waves and therefore seem not to be well suited to capture the long wave regime (see for instance [35] for similar results for the Boussinesq system in the KdV-KdV case).…”
Section: Former Well-posedness Resultsmentioning
confidence: 99%
“…The estimates derived in the aforementioned papers are not uniform 4 in µ. However, a recent study by Tesfahun [49] proved that the system corresponding to (1.7) in the 2-dimensional case and without surface tension is well-posed on a time interval of order O( 1 √ ε ) in the KdV−regime. Indeed, dispersive techniques are tailored-made for short waves and therefore seem not to be well suited to capture the long wave regime (see for instance [35] for similar results for the Boussinesq system in the KdV-KdV case).…”
mentioning
confidence: 96%