Model:PyDeltaRCM: Difference between revisions
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|Spatialscale=Landscape-Scale | |Spatialscale=Landscape-Scale | ||
|One-line model description=Reduced complexity river delta formation and evolution model with channel dynamics | |One-line model description=Reduced complexity river delta formation and evolution model with channel dynamics | ||
|Extended model description=pyDeltaRCM is the Python version of | |Extended model description=pyDeltaRCM is the Python version of DeltaRCM (https://csdms.colorado.edu/wiki/Model:DeltaRCM) by Man Liang (also available from the CSDMS model repository). This version is a WMT component but can also be run as a stand-alone model (see README.md). | ||
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. | 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. | Best usage of DeltaRCM is the investigation of autogenic processes in response to external forcings. |
Revision as of 10:55, 15 September 2020
PyDeltaRCM
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