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Modified Energy Functionals and the NLS Approximation
Analysis of PDEs · Submitted 31 May 2016
abstract compiled · 2026-09-23 · no language-model review
The authors' main claim We give a new proof of the fact that wave packet solutions of this equation are approximated by the nonlinear Schrodinger equation.
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The abstract, sentence by sentence
We consider a model equation from [14] that captures important properties of the water wave equation. We give a new proof of the fact that wave packet solutions of this equation are approximated by the nonlinear Schrodinger equation. This proof both simplifies and strengthens the results of [14] so that the approximation holds for the full interval of existence of the approximate NLS solution rather than just a subinterval. Furthermore, the proof avoids the problems associated with inverting the normal form transform in [14] by working with a modified energy functional motivated by [1] and [8].
background contribution method result interpretation main claim
| # | sentence | role | the authors' own work | states the main conclusion | strength |
|---|---|---|---|---|---|
| s0 | We consider a model equation from [14] that captures important properties of the water wave equation. | background 0.96 | 0.27 | 0.03 | asserted 1.00 |
| s1 | We give a new proof of the fact that wave packet solutions of this equation are approximated by the nonlinear Schrodinger equation. | contribution 0.85 | 0.95 | 0.71 | asserted 1.00 |
| s2 | This proof both simplifies and strengthens the results of [14] so that the approximation holds for the full interval of existence of the approximate NLS solution rather than just a subinterval. | result 0.79 | 0.93 | 0.65 | asserted 1.00 |
| s3 | Furthermore, the proof avoids the problems associated with inverting the normal form transform in [14] by working with a modified energy functional motivated by [1] and [8]. | method 0.81 | 0.87 | 0.09 | asserted 1.00 |
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The paper
Original abstract
We consider a model equation from [14] that captures important properties of the water wave equation. We give a new proof of the fact that wave packet solutions of this equation are approximated by the nonlinear Schrodinger equation. This proof both simplifies and strengthens the results of [14] so that the approximation holds for the full interval of existence of the approximate NLS solution rather than just a subinterval. Furthermore, the proof avoids the problems associated with inverting the normal form transform in [14] by working with a modified energy functional motivated by [1] and [8].
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