Hi,
since the last year we have some problems by simulation flushing events. In some simulations or in some areas of the mesh, we get "water surface striae" (see post
www.opentelemac.org/index.php/kunena/16-...-surface-striae#8282), which result due to the calculated shear stress in furrows in the evolution (
www.opentelemac.org/index.php/kunena/17-...n-the-evolution#5140).
I have this problem also with Telemac-3D internally coupled with Sisyphe. A water level difference of 1-2 cm gives differences of about 0.2-0.5 N/m2 in the TOB and causes differences in the evolution of 60-120cm (due to the small grain sizes ~1mm and the duration of 3 days).
I have already tried the bubble option, which helps a little bit and to change the free surface gradient (0.9 - 0.5 - 0.1), but this not much effect. It dumped the difference in evolution only about 5-10%.
Does anyone has some advice or hints?
Best regards,
Gabriele