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Rectification of a deep water model for surface gravity waves

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  • Additional Information
    • Contributors:
      Institut de Recherche Mathématique de Rennes (IRMAR); Université de Rennes (UR)-Institut National des Sciences Appliquées - Rennes (INSA Rennes); Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)-École normale supérieure - Rennes (ENS Rennes)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-INSTITUT AGRO Agrocampus Ouest; Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro); CEntre de REcherches en MAthématiques de la DEcision (CEREMADE); Université Paris Dauphine-PSL; Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS); ANR-20-CE40-0020,CRISIS,Régularité critique, interfaces, interactions multi-échelle et singularités dans la dynamique des fluides inhomogènes(2020)
    • Publication Information:
      HAL CCSD
      Mathematical Sciences Publishers
    • Publication Date:
      2024
    • Abstract:
      International audience ; In this work we discuss an approximate model for the propagation of deep irrotational water waves, specifically the model obtained by keeping only quadratic nonlinearities in the water waves system under the Zakharov/Craig--Sulem formulation. We argue that the initial-value problem associated with this system is most likely ill-posed in finite regularity spaces, and that it explains the observation of spurious amplification of high-wavenumber modes in numerical simulations that were reported in the literature. This hypothesis has already been proposed by Ambrose, Bona, and Nicholls (Proc. R. Soc. Lond., Ser. A, Math. Phys. Eng. Sci. 470, No. 2166, 2014) but we identify a different instability mechanism. On the basis of this analysis, we show that the system can be "rectified". Indeed, by introducing appropriate regularizing operators, we can restore the well-posedness without sacrificing other desirable features such as a canonical Hamiltonian structure, cubic accuracy as an asymptotic model, and efficient numerical integration. This provides a first rigorous justification for the common practice of applying filters in high-order spectral methods for the numerical approximation of surface gravity waves. While our study is restricted to a quadratic model, we believe it can be generalized to any order and paves the way towards the rigorous justification of a robust and efficient strategy to approximate water waves with arbitrary accuracy. Our study is supported by detailed and reproducible numerical simulations.
    • Relation:
      info:eu-repo/semantics/altIdentifier/arxiv/2203.03277; hal-03598747; https://hal.science/hal-03598747; https://hal.science/hal-03598747v2/document; https://hal.science/hal-03598747v2/file/RWW2v2.pdf; ARXIV: 2203.03277
    • Accession Number:
      10.2140/paa.2024.6.73
    • Online Access:
      https://doi.org/10.2140/paa.2024.6.73
      https://hal.science/hal-03598747
      https://hal.science/hal-03598747v2/document
      https://hal.science/hal-03598747v2/file/RWW2v2.pdf
    • Rights:
      info:eu-repo/semantics/OpenAccess
    • Accession Number:
      edsbas.90788885