<p>We overview the recent result [<CitationRef CitationID="CR3">3</CitationRef>, Theorem 1.1] about the high-frequency instability of pure gravity Stokes waves subject to longitudinal perturbations. The spectral bands of unstable eigenvalues away from the origin form a sequence of <i>isolas</i> parameterized by an integer <InlineEquation ID="IEq1"> <EquationSource Format="TEX">\( \texttt{p}\ge 2 \)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <mi mathvariant="monospace">p</mi> <mo>≥</mo> <mn>2</mn> </mrow> </math></EquationSource> </InlineEquation> for any value of the depth <InlineEquation ID="IEq2"> <EquationSource Format="TEX">\( \texttt{h}&gt; 0 \)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <mi mathvariant="monospace">h</mi> <mo>&gt;</mo> <mn>0</mn> </mrow> </math></EquationSource> </InlineEquation> such that an explicit coefficient <InlineEquation ID="IEq3"> <EquationSource Format="TEX">\(\beta _1^{(\texttt{p})}(\texttt{h}) \)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <msubsup> <mi>β</mi> <mn>1</mn> <mrow> <mo stretchy="false">(</mo> <mi mathvariant="monospace">p</mi> <mo stretchy="false">)</mo> </mrow> </msubsup> <mrow> <mo stretchy="false">(</mo> <mi mathvariant="monospace">h</mi> <mo stretchy="false">)</mo> </mrow> </mrow> </math></EquationSource> </InlineEquation> is not zero. In [<CitationRef CitationID="CR3">3</CitationRef>] it is proved that the map <InlineEquation ID="IEq4"> <EquationSource Format="TEX">\( \texttt{h}\mapsto \beta _1^{(\texttt{p})}(\texttt{h}) \)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <mi mathvariant="monospace">h</mi> <mo>↦</mo> <msubsup> <mi>β</mi> <mn>1</mn> <mrow> <mo stretchy="false">(</mo> <mi mathvariant="monospace">p</mi> <mo stretchy="false">)</mo> </mrow> </msubsup> <mrow> <mo stretchy="false">(</mo> <mi mathvariant="monospace">h</mi> <mo stretchy="false">)</mo> </mrow> </mrow> </math></EquationSource> </InlineEquation> is analytic and it is not identically zero for any <InlineEquation ID="IEq5"> <EquationSource Format="TEX">\( \texttt{p}\ge 2 \)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <mi mathvariant="monospace">p</mi> <mo>≥</mo> <mn>2</mn> </mrow> </math></EquationSource> </InlineEquation>, by showing that <InlineEquation ID="IEq6"> <EquationSource Format="TEX">\( \lim _{\texttt{h}\rightarrow 0^+}\beta _1^{(\texttt{p})}(\texttt{h}) = - \infty \)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <msub> <mo movablelimits="true">lim</mo> <mrow> <mi mathvariant="monospace">h</mi> <mo stretchy="false">→</mo> <msup> <mn>0</mn> <mo>+</mo> </msup> </mrow> </msub> <msubsup> <mi>β</mi> <mn>1</mn> <mrow> <mo stretchy="false">(</mo> <mi mathvariant="monospace">p</mi> <mo stretchy="false">)</mo> </mrow> </msubsup> <mrow> <mo stretchy="false">(</mo> <mi mathvariant="monospace">h</mi> <mo stretchy="false">)</mo> </mrow> <mo>=</mo> <mo>-</mo> <mi>∞</mi> </mrow> </math></EquationSource> </InlineEquation>. In this manuscript we compute the asymptotic expansion of <InlineEquation ID="IEq7"> <EquationSource Format="TEX">\(\beta _1^{(\texttt{p})}(\texttt{h}) \)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <msubsup> <mi>β</mi> <mn>1</mn> <mrow> <mo stretchy="false">(</mo> <mi mathvariant="monospace">p</mi> <mo stretchy="false">)</mo> </mrow> </msubsup> <mrow> <mo stretchy="false">(</mo> <mi mathvariant="monospace">h</mi> <mo stretchy="false">)</mo> </mrow> </mrow> </math></EquationSource> </InlineEquation>in the deep-water limit <InlineEquation ID="IEq8"> <EquationSource Format="TEX">\( \texttt{h}\rightarrow + \infty \)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <mi mathvariant="monospace">h</mi> <mo stretchy="false">→</mo> <mo>+</mo> <mi>∞</mi> </mrow> </math></EquationSource> </InlineEquation> –it vanishes exponentially fast to zero– for <InlineEquation ID="IEq9"> <EquationSource Format="TEX">\(\texttt{p}=2\)</EquationSource> <EquationSource Format="MATHML"><math> <mrow> <mi mathvariant="monospace">p</mi> <mo>=</mo> <mn>2</mn> </mrow> </math></EquationSource> </InlineEquation>, 3, 4.</p>

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On higher order isolas of unstable stokes waves

  • Massimiliano Berti,
  • Livia Corsi,
  • Alberto Maspero,
  • Paolo Ventura

摘要

We overview the recent result [3, Theorem 1.1] about the high-frequency instability of pure gravity Stokes waves subject to longitudinal perturbations. The spectral bands of unstable eigenvalues away from the origin form a sequence of isolas parameterized by an integer \( \texttt{p}\ge 2 \) p 2 for any value of the depth \( \texttt{h}> 0 \) h > 0 such that an explicit coefficient \(\beta _1^{(\texttt{p})}(\texttt{h}) \) β 1 ( p ) ( h ) is not zero. In [3] it is proved that the map \( \texttt{h}\mapsto \beta _1^{(\texttt{p})}(\texttt{h}) \) h β 1 ( p ) ( h ) is analytic and it is not identically zero for any \( \texttt{p}\ge 2 \) p 2 , by showing that \( \lim _{\texttt{h}\rightarrow 0^+}\beta _1^{(\texttt{p})}(\texttt{h}) = - \infty \) lim h 0 + β 1 ( p ) ( h ) = - . In this manuscript we compute the asymptotic expansion of \(\beta _1^{(\texttt{p})}(\texttt{h}) \) β 1 ( p ) ( h ) in the deep-water limit \( \texttt{h}\rightarrow + \infty \) h + –it vanishes exponentially fast to zero– for \(\texttt{p}=2\) p = 2 , 3, 4.