2020
DOI: 10.48550/arxiv.2010.14156
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Global bifurcation and highest waves on water of finite depth

Vladimir Kozlov,
Evgeniy Lokharu

Abstract: We consider the two-dimensional problem for steady water waves on finite depth with vorticity. While neglecting the effects of surface tension we construct connected families of large amplitude periodic waves approaching either a solitary wave, the highest solitary wave or the highest Stokes wave. In contrast to previous studies we fix the Bernoulli constant and consider the wavelength as a bifurcation parameter, which guarantees that the limiting wave has a finite depth. In fact, this is the first rigorous pr… Show more

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Cited by 4 publications
(15 citation statements)
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“…Then either (i) C ′ δ is unbounded in R × X, or (ii) C ′ δ contains another trivial point (t 1 , 0) with t 1 = t M , or (iii) C ′ δ contains a point (t, w) ∈ ∂O δ . In [15] it is proved an estimate Λ(t) ≥ c 0 > 0 for all t ∈ R, where the constant c 0 depends only on ω and r. This estimate implies λ(t) ≤ Λ(0) c 0 .…”
Section: Global Subharmonic Bifurcation Theoremsmentioning
confidence: 94%
“…Then either (i) C ′ δ is unbounded in R × X, or (ii) C ′ δ contains another trivial point (t 1 , 0) with t 1 = t M , or (iii) C ′ δ contains a point (t, w) ∈ ∂O δ . In [15] it is proved an estimate Λ(t) ≥ c 0 > 0 for all t ∈ R, where the constant c 0 depends only on ω and r. This estimate implies λ(t) ≤ Λ(0) c 0 .…”
Section: Global Subharmonic Bifurcation Theoremsmentioning
confidence: 94%
“…The only difference here is that the bifurcation parameter is the period and in verification of compactness and Fredholm properties in the global bifurcation theorem must be changed a little bit. We refer also to [9] and [10] where the assertion is proved for the unidirectional flows.…”
Section: Overhanging Free Surfacementioning
confidence: 99%
“…In order to overcome the inherited downsides of the above-mentioned semi-hodograph transformation and to allow for stagnation points and critical layers, many papers use a "naive" flattening transform, where on each vertical ray the vertical coordinate is scaled to a constant; see [1,21,23,24,31,35,37,47,50]. Consequently, a drawback of this naive flattening is that it needs the surface profile to be a graph and can thus not allow for overhanging waves.…”
Section: Introductionmentioning
confidence: 99%