Overslaan en naar de inhoud gaan
Publicaties | Personen | Instituten | Projecten
[ meld een fout in dit record ]mandje (0): toevoegen | toon Print deze pagina

Unstructured, anisotropic mesh generation for the Northwestern European continental shelf, the continental slope and the neighbouring ocean
Legrand, S.; Deleersnijder, E.; Delhez, E.J.M.; Legat, V. (2007). Unstructured, anisotropic mesh generation for the Northwestern European continental shelf, the continental slope and the neighbouring ocean. Cont. Shelf Res. 27(9): 1344-1356. dx.doi.org/10.1016/j.csr.2007.01.009
In: Continental Shelf Research. Pergamon Press: Oxford; New York. ISSN 0278-4343; e-ISSN 1873-6955, meer
Peer reviewed article  

Beschikbaar in  Auteurs 

Trefwoorden
    Analysis > Mathematical analysis > Numerical analysis > Finite element method
    Topographic features > Submarine features > Continental shelves
    Topographic features > Submarine features > Continental slope
    Marien/Kust
Author keywords
    unstructured grids; northwestern European continental shelf; Delaunay triangulation; finite elements methods; finite volumes methods

Auteurs  Top 
  • Legrand, S., meer
  • Deleersnijder, E., meer
  • Delhez, E.J.M., meer
  • Legat, V., meer

Abstract
    A new mesh refinement strategy for generating high quality unstructured meshes of the Northwestern European continental shelf, the continental slope and the neighbouring ocean is presented. Our objective is to demonstrate the ability of anisotropic unstructured meshes to adequately address the challenge of simulating the hydrodynamics occurring in these three regions within a unique mesh. The refinement criteria blend several hydrodynamic considerations as the tidal wave propagation on the continental shelf and the hydrostatic consistency condition in steep areas. Several meshes illustrate both the validity and the efficiency of the refinement strategy. The selection of the refinement parameters is discussed. Finally, an attempt is made to take into account tidal ellipses, providing another cause for anisotropy in the mesh.

Alle informatie in het Integrated Marine Information System (IMIS) valt onder het VLIZ Privacy beleid Top | Auteurs