Search by property
From CSDMS
This page provides a simple browsing interface for finding entities described by a property and a named value. Other available search interfaces include the page property search, and the ask query builder.
List of results
- Model:ParFlow + (Depends upon application.)
- Model:PyDeltaRCM + (Domain should be 10s of Kms in x and y. Cell spacing should be 10s of meters.)
- Model:FineSed3D + (Domain should be large enough to resolve the bottom boundary layer, meanwhile, the grid resolution should be fine enough to resolve all the essential turbulence scales.)
- Model:Kirwan marsh model + (Domain size is 3 km by 3 km, grid cell is 5 m by 5m.)
- Model:CruAKTemp + (Downsampled from original data to 10 km by 10 km resolution)
- Model:CosmoLand + (Drainage basin size controls the length of the model runs. Cell size should not be increased to shorten model runs.)
- Model:ROMS + (Estuary, regional, and basin scales. There are couple of global applications.)
- Model:ChesROMS + (Estuary, regional, and basin scales. There are couple of global applications.)
- Model:CBOFS2 + (Estuary, regional, and basin scales. There are couple of global applications.)
- Model:UMCESroms + (Estuary, regional, and basin scales. There are couple of global applications.)
- Model:TAo + (From continental to regional scale (>50 km). Up to a few thousand cells are well handled.)
- Model:ISSM + (From hundreds of meters to thousands of kilometers (constraints are mainly HEC-related).)
- Model:GSFLOW-GRASS + (GSFLOW is intended for modeling catchments from the km-scale to the 100s-of-km scale)
- Model:Caesar + (Has been applied to catchments ranging from 1km^2 to 500km^2, at grid resolutions ranging from 1m to 50m.)
- Model:GOLEM + (Has been used on scales from small (few km2) watersheds to sub-continental areas.)
- Model:WEPP + (Hillslope simulations are recommended for … Hillslope simulations are recommended for lengths not greatly exceeding 100 meters. Watershed simulations should not exceed areas above 260 hectares. Larger areas can be simulated for hillslope spatial analyses only - but the channel processes will not be accurate at these larger scales.ll not be accurate at these larger scales.)
- Model:Subside + (Horizontal resolution is typically 100s of meters)
- Model:Inflow + (Horizontal resolution is typically 10s of meters)
- Model:Sakura + (Horizontal resolution is typically 10s of meters)
- Model:FVshock + (Hundreds of Km (the reach of a river).)