Abstract
The Peregrine soliton \(Q(x,t)=e^{it}(1-\frac{4(1+2it)}{1+4x^2+4t^2})\) is an exact solution of the 1d focusing nonlinear Schrödinger equation (NLS) \(iB_t+B_{xx}=-2|B|^2B\), having the feature that it decays to \(e^{it}\) at the spatial and time infinities, and with peaks and troughs in a local region. It is considered as a prototype of the rogue wave by the ocean waves community. The 1D NLS is related to the full water wave system in the sense that asymptotically it is the envelope equation for full water waves. In this paper, working in the framework of water waves which decay non-tangentially, we give a rigorous justification of the NLS from the full water waves equation on long time scale in a regime that allows for the partial justification of the Peregrine soliton. As a byproduct, we prove the long time existence of solutions for the full water waves equation with small initial data in space of the form \(H^s(\mathbb {R})+H^{s'}(\mathbb {T})\), where \(s\geqq 4, s'>s+\frac{3}{2}\).
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Notes
By nonvanishing, we mean that the water wave is neither periodic nor at rest at spatial infinity.
Indeed, we need only \(k> 0\). If \(k\ne \mathbb {N}\), then \(e^{ik\alpha }\notin H^s(\mathbb {T})\), instead, it is in \(H^s(\mathbb {T}/k)\). For simplicity, we take \(k\in \mathbb {N}\). The same argument applies directly to the cases that \(k\ne \mathbb {N}\).
By localized waves. we mean those waves which are at rest at spatial infinity.
The letter \(\mathcal {N}\) means nontangentially, while the letter \(\mathcal {P}\) means periodic.
In this paper, by a function f decays at \(\infty \), we mean that \(f\in H^s(\mathbb {R})\) for some \(s\geqq 0\), even though it could be possible that \(\lim _{x\rightarrow \infty }f(x)\) does not exist.
This is in \(\infty \)-norm sense, i.e., \(\Vert \zeta -\tilde{\zeta }\Vert _{W^{s,\infty }}=O(\varepsilon ^4)\). In \(X^s\) norm, \(\Vert \zeta -\tilde{\zeta }\Vert _{X^s}=O(\varepsilon ^{7/2})\).
Here, the inner product on \(L^2(|\mathrm{d} \omega |)\) is given by \(\langle f, g\rangle _{L^2(|\mathrm{d}\omega |)}:=\int _{\mathbb {T}}f(\alpha )\overline{g(\alpha )}|\omega _{\alpha }|\mathrm{d}\alpha \).
Note that \(\mathcal {H}_{\zeta }b\) and \(\mathcal {H}_{\omega }b_0\) are defined as BMO functions. Moreover, \(\mathcal {H}_{\zeta }b-\mathcal {H}_{\omega }b_0\in H^s(\mathbb {R})\). Similar properties hold for other quantities such as \(A, A_0\).
See also the estimate for \(r_1\) in the next two sections. The estimates for \(r_0\) can be obtained parallel to the estimates for \(r_1\). The estimate for \(r_1\) is more involved and requires more careful analysis, so we present the details for the estimates of \(r_1\).
The meaning of essentially positive should be clear from Lemma 9.2.
Because \(U_2\) is completely determined by \(\omega \) and B, which are controlled over \(O(\varepsilon ^{-2})\) time scale.
\((I-\mathcal {H}_{\zeta })\partial _{\alpha }^{n+1}\rho _1\) and \((I-\mathcal {H}_{\zeta })\overline{\partial _t\mathcal {R}_1^{(n)}}\) are boundary value of holomorphic functions in \(\Omega (t)^c\).
Write \(r_1=\frac{1}{2}(I+\mathcal {H}_{\zeta })r_1+\frac{1}{2}(I-\mathcal {H}_{\zeta })r_1\). Use the argument in Lemma 8.3, we can show that \(\left\Vert \partial _{\alpha }(I+\mathcal {H}_{\zeta })r_1\right\Vert _{H^s}\leqq C(\varepsilon E_s^{1/2}+\varepsilon ^{5/2})\).
Recall that \(\xi =\zeta -\alpha \), \(\tilde{\xi }=\tilde{\zeta }-\alpha \), \(\xi _0=\omega -\alpha \), and \(\tilde{\xi }_0=\tilde{\omega }-\alpha \).
Let k be any nonzero constant, then the lemma still holds, but we need to replace \(W^{s'+1,\infty }(\mathbb {T})\) by \(W^{s'+1,\infty }(\frac{\mathbb {T}}{k})\)
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Acknowledgements
The author would like to thank his Ph.D. advisor, Prof. Sijue Wu, for introducing him to this interesting topic, for many helpful discussions and invaluable comments. The author would like to thank the anonymous referee for many helpful suggestions. The author would like to thank Prof. Peter Miller and Prof. Rauch for intriguing discussions on rogue waves and NLS with nonzero boundary conditions. The author would also like to thank Fan Zheng and S. Shahshahani for invaluable comments, and Prof. Tao Luo for reading the draft of this paper. This work was partially supported by NSF Grant DMS-1361791.
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Appendices
Appendix A. Holomorphicity of Plane Waves
Let \(\zeta (\alpha )=\alpha +ce^{ik\alpha }, \alpha \in \mathbb {R}\), c is a small constant, \(k>0\), for simplicity, assume k is an integer. Let
Then \(\Gamma \) is a graph. Let \(\Omega _+\) be the region above \(\Gamma \), and \(\Omega _-\) the region below \(\Gamma \). On one hand, it is easy to prove
Lemma A.1
\(\alpha \), \(e^{-ik\alpha }\) and \(e^{ik\alpha }\) are holomorphic in \(\Omega _+\).
On the other hand, we’ll show that \(e^{ik\alpha }\) cannot be a boundary value of a bounded holomorphic function in \(\Omega _-\).
Lemma A.2
If \(c\ne 0\), then \(e^{ik\alpha }\) cannot be a boundary value of a holomorphic function in \(\Omega _-\).
Proof
If \(e^{ik\alpha }\) is a boundary value of a holomorphic function in \(\Omega _-\), then \(e^{ik\alpha }\) is complete, and so \(\alpha \) is as well. Assume that \(\alpha =\Phi (\zeta (\alpha ))\), \(\Phi \) being complete. Let \(\Psi (\zeta )=\zeta +ce^{ik\zeta }\). Then \(\Psi \) is complete, and \(\Psi (\alpha )=\zeta (\alpha )\). Thus we have
\(\Psi \circ \Phi \) and \(\Phi \circ \Psi \) are complete, so we must have \(\Psi \circ \Phi (z)\equiv z, \Phi \circ \Psi (z)\equiv z\). Thus \(\Psi \) and \(\Phi \) are the inverse of each other.
If \(c\ne 0\), then the function \(z+ce^{ikz}\) has an essential singularity at \(\infty \) because \(ce^{ikz}\) does. By Picard’s theorem, \(z+ce^{ikz}\) attains all values in \(\mathbb {C}\) infinitely many times with at most one exception. Suppose \(z_0\) is this exception, i.e., \(z+ce^{ikz}=z_0\) has finitely many solutions (possibly none). Then \(z+ce^{ikz}=z_0+2\pi \) has infinitely many solutions. Then
Thus \(z+ce^{ikz}=z_0\) has infinitely many solutions, which is a contradiction.
In particular, \(z+ce^{ikz}=0\) has infinitely many solutions. Thus \(\Psi \) is not invertible, which is a contradiction. \(\square \)
Lemma A.3
If \(e^{-ik\alpha }\) is boundary value of a holomorphic function in \(\Omega _-\), then \(e^{ik\alpha }\) is also holomorphic in \(\Omega _-\).
Proof
Let \(e^{-ik\alpha }=G(\zeta (\alpha ))\), where G is holomorphic in \(\Omega _-\). Then the zeros of G are a discrete set, which we denote by S. We’ll show that \(S=\emptyset \). Since \(\zeta =\alpha +ce^{ik\alpha }\), we have
Define\(H(\zeta ):=\zeta -\frac{c}{G(\zeta )}, ~ \zeta \in \Omega _-\). Then H has boundary value \(\alpha \). Thus \(\alpha \) is boundary value of a meromorphic function in \(\Omega _-\), with poles at S.
Note that \(e^{-ikH(\zeta (\alpha ))}\) has boundary values \(e^{-ik\alpha }\), and \(e^{-ikH(\zeta )}\) is holomorphic in \(\Omega _-\setminus S\), by uniqueness extension of holomorphic functions, we must have \(e^{-ikH(\zeta )}=G(\zeta )\) on \(\Omega _-\setminus S\).
If \(S\ne \emptyset \), then take \(z_0\in S\). Then since \(G(z_0)\) is defined, \(z_0\) must be a removable singularity of \(e^{-ikH(\zeta )}\). However, since \(z_0\) is a pole of \(H(\zeta )\), so \(z_0\) is an essential singularity of \(e^{-ikH(\zeta )}\), which is a contradiction. Thus \(S=\emptyset \).
We conclude that \(\alpha \) is holomorphic in \(\Omega _-\), and so \(e^{ik\alpha }\) is holomorphic in \(\Omega _-\). \(\square \)
Corollary A.1
\(e^{-ik\alpha }\) cannot be the boundary value of a holomorphic function in \(\Omega _-\) if \(c\ne 0\).
Appendix B
As before, we use the periodic Hilbert transform to estimate the error term \(r_0\). The nonlocal Hilbert transform \(\mathcal {H}_{\omega }\) is used when we estimate the error term \(r_1\). Let’s denote \(\tilde{\mathfrak {H}}_p\) as the periodic Hilbert transform associated with \(\tilde{\omega }\).
1.1 B.1 Governing Equation for \(r_0\)
We have
We split \(\mathcal {G}\) as \(\mathcal {G}=\mathcal {G}_1+\mathcal {G}_2+\mathcal {G}_3+\mathcal {G}_4\), where
and
and
1.2 B.2 Governing Equation for \(D_t^0(I-\mathfrak {H}_p)r_0\)
We need to derive an equation to control \(D_t^0 r_0\) as well. We consider instead the quantity
We have
and
Using (489) and (490), we have that
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Su, Q. Partial Justification of the Peregrine Soliton from the 2D Full Water Waves. Arch Rational Mech Anal 237, 1517–1613 (2020). https://doi.org/10.1007/s00205-020-01535-1
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DOI: https://doi.org/10.1007/s00205-020-01535-1