Hi,
I'm still trying to run a sediment transport triggered by a tsunami. Now, I increased the area of the mesh to test a new case and achieved a simulation with only suspended load. However, when I checked the BED EVOLUTION result, it showed this showed variations only in a small area, as shown in image 1. I would expect there would be widespread variation across all small bays following a similar pattern of the BED SHEAR STRESS result, but this wasn't the case. What could be the reason for this? Do I need to modify something in the steering file?
On the other hand, I still can't run the model using bedload or both together. Starting at iteration 360, modelling starts by exceeding the maximum iterations and then displays the NaN values. My model uses a TIDAL FLAT option, so following the manual's recommendations and some posts on this forum, I tried 13 or 14 for the SCHEME FOR ADVECTION OF VELOCITIES/ K-EPSILON, but it didn't work. Also, I tried the other options and got the same problem. Any recommendations on what I might have been doing wrong would be a great contribution to my project.
Please find attached all the files needed to run my problem.
Thank you in advance,
Cheers
Tomas