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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:GLUDM + (At the moment the resolution of the input controls the resolution of the output. This is a global model but can be applied to smaller domains.)
- Model:WBMsed + (Available datasets are for global and continental domains. Realistic high-res simulations for global scale is 6 arc-min and for continental 3 arc-min. Higher resolution datasets are available for both (e.g. 15 arc-sec for Europe).)
- Model:GEOMBEST++ + (Cell length - 10 - 100 meters Cell height - 0.01 - 0.5 meters)
- Model:GEOMBEST++Seagrass + (Cell length: 10 - 100 m (typically 50 m) Cell height 0.01 - 0.5 m (typically (0.1 m))
- Model:CarboLOT + (Cells are approximately 1-1000m in scale; map areas 10-100km on side.)
- Model:Barrier Inlet Environment (BRIE) Model + (Coastal barrier ~10-100 km length scales, and ~100 m alongshore resolution. Parameterizations not suitable for small-scale (tidal inlet etc) analyses)
- Model:RASCAL + (Code has been most commonly run for 10x5 m … Code has been most commonly run for 10x5 m cells (with the long axis parallel to flow) and domain size of 1.27 x 1.86 km. Other scales are possible, but adding additional cells will slow down processing. This model is only designed to simulate mean flows; resolution of fine turbulence structure is not possible with the code.e structure is not possible with the code.)
- Model:Area-Slope Equation Calculator + (Computer memory.)
- Model:GEOMBEST-Plus + (Constraints: * Cell length - 10 - 100 meters * Cell height - 0.01 - 0.5 meters)
- Model:BarrierBMFT + (Cross-shore transect length can extend 10's of km from the ocean barrier shoreface into the mainland. Grid resolution on the barrier is 10 m, and 1 m spacing from the back-barrier marsh to the mainland.)
- Model:CAM-CARMA + (Currently there are only initial data sets for 10x15 degrees longitude and latitude. This model is meant for global scale dynamics.)
- Model:WACCM-EE + (Currently, 4x5 degree, with 66 vertical levels up to 140 km. Resolution can be increased if neccessary)
- Model:Avulsion + (Delta-scale)
- Model:GSSHA + (Dependent upon computational power and memory.)
- Model:Landlab + (Depends on application/process)
- 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).)
- Model:HydroTrend + (HydroTrend should be applied to river larger than 100km; and basins smaller than 75000km2.)
- Model:Pllcart3d + (In its current state, the code is restricted to low Reynolds number and Peclet number of order 1000.)
- Model:CHILD + (In principle, the model can address spatia … In principle, the model can address spatial scales ranging from gullies and small (~1km2) catchments to mountain ranges, as long as setup and parameters are chosen appropriately. Resolutions greater than about 10,000 nodes normally require significant computation time.ally require significant computation time.)
- Model:Quad + (In the field, this model is applicable in the range of landscape and regional scales (~10-100km). It has also been successfully applied at the scale of physical experiments.)
- Model:IDA + (Increasing the number of processors should allow larger/higher resolution landscapes to be considered.)
- Model:RivMAP + (Input channel masks can be arbitrary resolution)
- Model:HexWatershed + (It is best performance for high resolution (<100m) simulation. With the version 3.0, coarser resolution is supported through stream burning feature.)
- Model:TOPOG + (It is intended for application to small catchments (up to 10 km2, and generally smaller than 1 km2).)
- Model:Morphodynamic gravel bed + (It's a reach scale. It is applied to 30km downstream of the Buech river. However, if dx is changed upward/downward, the time step should be adjusted.)
- Model:CEM + (Kilometers to hundreds of kilometers. Numerically, the model can be discretized with much smaller spatial resolution. However, the assumptions of approximately shore-parallel shoreface contours becomes unreasonable at scales smaller than kilometers.)
- Model:LISFLOOD + (LISFLOOD is grid-based, and applications so far have employed grid cells of as little as 100 metres (for medium-sized catchments), to 5,000 metres for modelling the whole of Europe and up to 0.1° (around 10 km) for modelling on a global scale.)
- Model:CASCADE + (Large scale (100 km+) model, suitable for orogenic scale modeling but could easily be adapted)
- Model:SPACE + (Length scale should be reach or larger (~100m and up). Run time depends on grid size and resolution.)
- Model:ErosionDeposition + (Length scale: ~10's of meters to ~1000's of km)
- Model:TUGS + (Length varies, resolution is on the order of several channel width (i.e., 1D model produces only reach-averaged results).)