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Mercredi 17 août 2005

Ref/Dif is a wave propagation model developped by the Center for Applied Coastal Research of the University of Delaware. It is used to provide the circulation model (Shorecirc) with the wave forcing needed to move bodies of water.

Provided variables are:

wave height and direction, wave dissipation rate, wave breaking index, wave mass flux, wave celerity, group speed...

Also, one important information when studying sediment transport is wave orbital velocity, wich is the dominant factor affecting sediment resuspension in the Gulf of Lions.

   

Bottom sediment resuspension under wave orbital speeds. 

 

 

Ref/Dif stands for refraction and diffraction, two phenomena which are taken into account in the propagation equation of the waves. Waves thus undergo realistic transformations when approaching the shore even over complex bathymetries (refraction over rocky shelves or crescentic sand bars, diffraction by breakwaters or jetties...).

Reflection is not included, however. Since studied sites are dissipative beaches (i.e. beaches with weak slopes), this phenomenon is of a lesser importance.



Simulation of today's wave height around the Var region (south of France), courtesy of SurfOuest.

par Nans publié dans : oceane
 
 
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