Linear theory of wave generation by a moving bottom

Abstract : The computation of long wave propagation through the ocean obviously depends on the initial condition. When the waves are generated by a moving bottom, a traditional approach consists in translating the ``frozen'' sea bed deformation to the free surface and propagating it. The present study shows the differences between the classical approach (passive generation) and the active generation where the bottom motion is included. The analytical solutions presented here exhibit some of the drawbacks of passive generation. The linearized solutions seem to be sufficient to consider the generation of water waves by a moving bottom.
Liste complète des métadonnées


https://hal.archives-ouvertes.fr/hal-00114954
Contributeur : Denys Dutykh <>
Soumis le : dimanche 19 novembre 2006 - 20:38:54
Dernière modification le : jeudi 9 février 2017 - 15:29:31
Document(s) archivé(s) le : mardi 6 avril 2010 - 23:04:24

Fichiers

final.pdf
Fichiers produits par l'(les) auteur(s)

Licence


Distributed under a Creative Commons Paternité 4.0 International License

Identifiants

Collections

Citation

Denys Dutykh, Frédéric Dias, Youen Kervella. Linear theory of wave generation by a moving bottom. Comptes rendus hebdomadaires des séances de l'Académie des sciences, Elsevier, 2006, 343, pp.499-504. <http://www.sciencedirect.com/science/article/pii/S1631073X06003657>. <10.1016/j.crma.2006.09.016>. <hal-00114954>

Partager

Métriques

Consultations de
la notice

275

Téléchargements du document

128