Closed krober10nd closed 3 years ago
Interesting! I'll check it out later.
I played around with the other forcing function a little bit and found virtually no improvement. Not sure what the difference to your observations is.
When building so-called geophysical multiscale meshes with orders of magnitude (like 100-m to 10 km in one domain) variations in mesh size, it converged faster than the Persson-Strang function.
What were your test cases?
Maybe try the rectangle with refinement case
I tried with a disk mesh. If it's not better for that, I have little hope for other domains tbh.
I observed it influenced the rate of convergence of mesh quality. I'd like to run some comparisons at some point and will post them here or on Sm. Feel free to close it of course. Just found the paper interesting.
I observed it influenced the rate of convergence of mesh quality.
The mesh quality is almost always 98% and more because the starting grid is so good. I'm not sure how you measure a faster rate of convergence.
imp_distmesh2d.pdf