You can send a PM or post an image of the mesh with depths. A few remarks:
Tomawac:
- Timestep is too large for braking waves. Make sure this rule is obeyed (extract from another post in the forum, I keep it in hand):
- Consider coupling Tomawac. Such big evolutions do not justify steady wave conditions
As rule of thumb, you should set the time step in order to have a Courant number between 1 and 2.
The Courant number Cr is given by : Cr=Cg(fp)*Dt//Dx
Where Cg(fp) is the group velocity associated to
the peak frequency, Dt is the time step and Dx is the size of the
smallest element of the spatial mesh.
The group velocity can be calculated from the dispersion relation. In
the deep water case, the group velocity is approximately equal to 0.78/fp, while in shallow waters Cg=(g*d)0.5, where g is the gravity acceleration and d is the water depth.
Sisyphe:
- Timestep is also big (10s). See if reducing it softens the evolution.
- Make use of SLOPE EFFECT to 'smooth' evolution by using a mild FRICTION ANGLE OF THE SEDIMENT
- Since you are using suspension, choose ADVECTION SCHEME 14 (similarly to Telemac3D)
Telemac:
- Try reducing the coupling period with Sisyphe. Work your way up from 1
Your mesh is quite coarse. See that it justifies the Courrant criterion for TOM.
Regards,
Costas