Filters the last few grid points after the physically-based inversion.
For various reasons (but mostly: the equilibrium assumption), the last few grid points on a glacier flowline are often noisy and create unphysical depressions. Here we try to correct for that. It is not volume conserving, but area conserving.
the glacier directory to process
- Files written to the glacier directory:
List of dicts containing the output data from the inversion.