Closed alimaye closed 1 year ago
Yeah, I can take a crack at this. The timing will be asynchronous with the timing of saved model states, but it should be possible to get them to line up close enough to test the idea. I'll have to redo all of the model runs, though, which may take a bit of time (so likely not before we discuss Thursday)
@amoodie Started thinking through how we can explain the differing deposit geometries for no-water vs. water. It seems like it has to be a difference in the avulsion locations: I'd guess avulsions are more common at the edge of the deposit for no-water, leading to propagation individual strands; whereas for the water case deposition at the water boundary might cause backfilling and avulsion upstream.
Can we test this by plotting avulsion locations through time (e.g., with a marker on the source cell in the movies?) Perhaps with a slight tweak
propagateAvulsion.m
can spit out time steps and locations for avulsion paths to file.