DeltaRCM is a parcel-based cellular flux routing and sediment transport model for the formation of river deltas, which belongs to the broad category of rule-based exploratory models. It has the ability to resolve emergent channel behaviors including channel bifurcation, avulsion and migration. Sediment transport distinguishes two types of sediment: sand and mud, which have different transport and deposition/erosion rules. Stratigraphy is recorded as the sand fraction in layers. Best usage of DeltaRCM is the investigation of autogenic processes in response to external forcings.
delta evolution, cellular automata, coastal morphodynamics,
Python
Modify water/sediment discharge (as number of parcels), grid size and spacing, basin geometry, mud/sand ratio, etc
- PNG files of eta, stage, depth - grids of eta, stage, depth (as netCDF4) - grids of sand fraction in stratigraphy (as netCDF4)
This part will be filled out by CSDMS staff
See more publications of PyDeltaRCM