2016
DOI: 10.1016/j.crma.2016.03.004
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On the existence and qualitative theory of stratified solitary water waves

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Cited by 26 publications
(78 citation statements)
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“…which is of the form R = −P − ψ M where P is the pressure and we choose M := γ . Using Yih's equation we find that in , the function R satisfies: Note, this is the equation derived in [1], Proposition 4.1. However, since ψ Y < 0 on ∪ B, the righthand side of (82) is strictly positive.…”
Section: Overhanging Wavesmentioning
confidence: 74%
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“…which is of the form R = −P − ψ M where P is the pressure and we choose M := γ . Using Yih's equation we find that in , the function R satisfies: Note, this is the equation derived in [1], Proposition 4.1. However, since ψ Y < 0 on ∪ B, the righthand side of (82) is strictly positive.…”
Section: Overhanging Wavesmentioning
confidence: 74%
“…carefully verify that the added stratification term does not cause too many complications. Indeed, in past literature, one major difficulty of proving nodal properties for stratified waves lies in the fact that the zeroth order term generally has the wrong sign (for example, see [1,3]).…”
Section: Monotonicity Propertiesmentioning
confidence: 99%
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“…Very recently, two of the authors provided the first construction of large-amplitude solitary waves with arbitrary (smooth and stable) stratification and background current [10,11]. In the present paper, however, we merely focus on periodic traveling waves.…”
Section: Surface Waves With Continuous Stratificationmentioning
confidence: 99%
“…These bifurcation methods, however, cannot give a qualitative description of the obtained solutions as they rely upon topological arguments. Only based on a thorough analysis of the underlying equations, a priori estimates and bounds on physical quantities have been derived in different settings of the water-wave problem, both with and without vorticity [8,9].…”
Section: Introductionmentioning
confidence: 99%