SPH Simulation of Onshore Bores with Counter Rotational Vortical Structure (Contributo in atti di convegno)

Type
Label
  • SPH Simulation of Onshore Bores with Counter Rotational Vortical Structure (Contributo in atti di convegno) (literal)
Anno
  • 2005-01-01T00:00:00+01:00 (literal)
Alternative label
  • Landrini, Maurizio Colagrossi, Andrea Greco, Marilena Tulin, Marshall Peter (2005)
    SPH Simulation of Onshore Bores with Counter Rotational Vortical Structure
    in 20th International Workshop on Water Waves and Floating Bodies (20th IWWWFB), Longyearbyen, Norway, 29 May 1 June 2005
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Landrini, Maurizio Colagrossi, Andrea Greco, Marilena Tulin, Marshall Peter (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#titoloVolume
  • 20th International Workshop on Water Waves and Floating Bodies (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 4 (literal)
Note
  • PuM (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • INSEAN Ocean Engineering Laboratory, UCSB, S. Barbara, CA, USA (literal)
Titolo
  • SPH Simulation of Onshore Bores with Counter Rotational Vortical Structure (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#curatoriVolume
  • J. Grue (Univeristy of Oslo) (literal)
Abstract
  • The generation and evolution of two-dimensional bores are analyzed numerically by using the Smoothed Particle Hydrodynamics (SPH) method. With this tool the bore steepening, breaking and post-breaking phases have been detailed investigated in the cases of constant and variable water depths. The bores were generated through a piston wavemaker moving with constant speed and the flow features have been studied by varying the water-depth Froude number from 0.5 to 0.95. The breaking of a plunging bore on the underlying water injects a cyclic process of splashes up with different strengths. The analysis highlighted also the occurrence of clockwise and anti-clockwise vortices, later pairing to form dipole structures. These affect the water evolution and can interact in a complex way with the free surface and with the sea floor. In the latter case, large stresses can be induced at the bottom that are responsible for instance for erosion. (literal)
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