Multilayer Saint-Venant Model with Variable Density
Response of a stratified lake to wind stress
Temperature stratification with
Tepi = 20 ° C, Thypo = 7 ° C,
Tmeta = linear variation.
Vwind = 15 m/s.
Wind stopped after 18 hours.
E. Audusse, M.-O. Bristeau, M. Pelanti, and
J. Sainte-Marie, Approximation of the hydrostatic Navier-Stokes system for
density stratified flows by a multilayer model:
Kinetic interpretation and numerical solution,
J. Comput. Phys., 230:9, 3453-3478, 2011.
E. Audusse, M.-O. Bristeau, B. Perthame and J. Sainte-Marie,
A multilayer Saint-Venant system with mass exchanges for Shallow Water flows,
M2AN, 45, 169-200, (2010).
This work has been carried in the framework of a joint research project
between the INRIA team BANG and the
French National Laboratory of Hydraulics and Environment
and Development). Principal collaborators:
M.-O. Bristeau (INRIA),
J. Sainte-Marie (INRIA and LNHE-EDF),
M.-J. Salençon (EDF R&D).