Three-dimensional numerical modeling of flows over a natural dune field
Détails
ID Serval
serval:BIB_74211169B83C
Type
Actes de conférence (partie): contribution originale à la littérature scientifique, publiée à l'occasion de conférences scientifiques, dans un ouvrage de compte-rendu (proceedings), ou dans l'édition spéciale d'un journal reconnu (conference proceedings).
Collection
Publications
Institution
Titre
Three-dimensional numerical modeling of flows over a natural dune field
Titre de la conférence
River Flow 2006, Vols 1 and 2
ISBN
0-415-40815-6
Statut éditorial
Publié
Date de publication
2006
Editeur⸱rice scientifique
Ferreira RML, Alves CTL, Leal GAB, Cardoso AH
Série
Proceedings and Monographs in Engineering, Water and Earth Sciences
Pages
1077-1083
Notes
International Conference on Fluvial Hydraulics, Lisbon, PORTUGAL, SEP
06-08, 2006
06-08, 2006
Résumé
Our ability to numerically predict the interaction between complex
topography and three dimensional flow at large scales (similar to 1 km)
has yet to be fully developed. This is the result of our inability to
design numerically stable meshes for complex topographies at these
spatial resolutions. This paper deals with the numerical simulation of
flow over a natural dune field located in the Rio Parana, NE Argentina.
The methodology is based upon the development and application of a new
five term porosity algorithm that modifies the mass conservation
equation within a regular Cartesian mesh. Bathymetric measurements were
made in the field using a multibeam echo sounder which provided an
unparalleled topographic dataset to test this new numerical modeling
approach. Measurements of flow were made using an acoustic Doppler
current profiler and are used as inlet boundary conditions and
validation data. The results demonstrate simple flow acceleration due
to topographic forcing over the dune stoss and expansion and
deceleration over the dune lee.
topography and three dimensional flow at large scales (similar to 1 km)
has yet to be fully developed. This is the result of our inability to
design numerically stable meshes for complex topographies at these
spatial resolutions. This paper deals with the numerical simulation of
flow over a natural dune field located in the Rio Parana, NE Argentina.
The methodology is based upon the development and application of a new
five term porosity algorithm that modifies the mass conservation
equation within a regular Cartesian mesh. Bathymetric measurements were
made in the field using a multibeam echo sounder which provided an
unparalleled topographic dataset to test this new numerical modeling
approach. Measurements of flow were made using an acoustic Doppler
current profiler and are used as inlet boundary conditions and
validation data. The results demonstrate simple flow acceleration due
to topographic forcing over the dune stoss and expansion and
deceleration over the dune lee.
Web of science
Création de la notice
03/02/2011 15:40
Dernière modification de la notice
20/08/2019 15:31
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