TISC is a code to model isostasy, erosion/sediment transport/sedimentation, and tectonic kinematics, mostly for the study of sedimentary basins and source to sink systems.
If you can see in most of the time steps (most predominately in 6.0 Ma as cross section is on a point). You can see that we have a single grid point that creates an anomaly. One point is higher than the other points, and it only lasts temporally, but they are in most time steps. We have used several combinations of Nx, Ny, dt, and eros_dt and we will still get these misbehaving points.
These only happen when we have erosional processes on.
Any suggestions on eliminating these?
Also, we are getting "jagged" sediments as open a rift, most apparent is 7 Ma and 8 Ma in the crosssection. Is there anything that can be done to make these appear more realistic?
If you can see in most of the time steps (most predominately in 6.0 Ma as cross section is on a point). You can see that we have a single grid point that creates an anomaly. One point is higher than the other points, and it only lasts temporally, but they are in most time steps. We have used several combinations of Nx, Ny, dt, and eros_dt and we will still get these misbehaving points.
These only happen when we have erosional processes on.
Any suggestions on eliminating these?
Also, we are getting "jagged" sediments as open a rift, most apparent is 7 Ma and 8 Ma in the crosssection. Is there anything that can be done to make these appear more realistic?