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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:QDSSM  + (The model has been successfully used for s … The model has been successfully used for simulation of river-shelf-slope configuration with a length of 0.005–400 km. The very short length scale refers to laboratory produced physical landscape models that have been used for calibration of avulsion and headward erosion processes.f avulsion and headward erosion processes.)
• Model:Alpine3D  + (The model has been used with cells from 5 meters up to kilometers scale.)
• Model:WDUNE  + (The model is abstract. Ratio of height to horizontal distance resolution is locked at 0.1, but can be modified in the source code and re-compiling.)
• Model:SWEHR  + (The model is designed to be used at the watershed scale or smaller.)
• Model:LateralVerticalIncision  + (The model is made of a series (5 to 100) of across-river profiles to model a river reach ca. 5 to 50 km in length and 1 to 20 km in width.)
• Model:Barrier3D  + (The model operates over a 10-by-10 m grid; the alongshore length of the barrier segment can range from hundreds to thousands of meters.)
• Model:OverlandFlow  + (The model works best at watershed-scale domains, 100 km^2 and less have been tested. Of course, this is highly dependent on the grid resolution.)
• Model:River Network Bed-Material Sediment  + (The river network is composed of links, defined as a segment of river channel between tributaries, but can be made smaller if desired. Generally each link has a length on the order of a few kilometers.)
• Model:Nitrate Network Model  + (The river network is composed of links, defined as a segment of river channel between tributaries, but can be made smaller if desired. Generally each link has a length on the order of a few kilometers.)
• Model:WAVEWATCH III ^TM  + (Theoretically length scale larger than longest wave length (10km), practically highest resolution sub km. Largest scales should correspond to spatial scales of forcing.)
• Model:CellularFanDelta  + (There are two primary constraints: # Like … There are two primary constraints:</br># Like most topographically-routed cellular river models, incised channels in the model will always be one cell wide. Hence it should not be applied at scales where the cell size is much less than main channel widths.</br># The model does not really simulate low-Froude low-slope rivers such as most large coastal deltas. However processes are similar to many other codes (e.g. DIONISOS) commonly used for large-scale deltas. If primary questions are about large-scale basin filling on O(10 ka) or longer timescales the model should be fine. However when questions relate to details of sub-millenial geomorphic processes or reservoir-scale stratigraphic architecture, some care must be taken in interpreting model results.st be taken in interpreting model results.)
• Model:Frost Model  + (There is no specific length scale and resolution to the index, as long as temperature conditions remains similar over the scale.)
• Model:DrEICH algorithm  + (This algorithm attempts to identify channe … This algorithm attempts to identify channel head, which are features present on a metre to sub-metre scale. Therefore, the accuracy of the prediction will decrease as the DEM resolution becomes coarser. 1 to 2m resolution DEMs are suggested as appropriate for use with this tool.ted as appropriate for use with this tool.)
• Model:Hilltop flow routing  + (This algorithm attempts to measure individual hillslopes, which are can be resolved at a range of spatial scales. It is recommended to use high resolution topographic data (<4 meter resolution) to ensure that a broad range of hillslopes can be sampled.)
• Model:GISKnickFinder  + (This code currently only works on a single watershed.)
• Model:SoilInfiltrationGreenAmpt  + (This component has been tested on the reach and watershed scale (<= 100 km^2), but can likely run effectively on even larger scales as needed.)
• Model:OceanWaves  + (This is a point model and not dependent on length scale or resolution.)
• Model:BRaKE  + (This model is intended for a CHANNEL REACH of CONSTANT DRAINAGE AREA.)
• Model:GullyErosionProfiler1D  + (This works for channels of hundreds of meters with 1 m cells)
• Model:CMFT  + (Transect length about 500 m)
• Model:Coastal Landscape Transect Model (CoLT)  + (Transect model with landscape of ~10 km (5 km bay, 1 km marsh, and 4 km forest in base version), 1 m grid scale horizontally.)
• Model:CSt ASMITA  + (Typical applications involve coastal syste … Typical applications involve coastal systems tens to hundreds of kilometers in extent. Very useful when there are many components in the coastal system. Although the gridded portion of the model usually use delta x and y values on the order of 100s of meters there is a sub-grid scale representation of the shoreline position with resolution of meters.reline position with resolution of meters.)
• Model:Erode  + (Typical grid cell dimensions are 10 to 500 meters.)
• Model:Cliffs  + (Typical resolution for open-ocean propagation: 2-4 arc-min, near the coast: 30-1 arc-sec; for lab experiments: tens to few cm.)
• Model:Non Local Means Filtering  + (Typically applied to high resolution (1 m LiDAR) gridded topographic datasets. Could pheasably be applied to other resolutions where the scale of noise is similar to the resolution of the topographic data.)

• Model:BOM  + (Uniform horisontal resolution, i.e. works best for resolutions < 20km.)

• Model:GRLP  + (Valid so long as the whole modeled region is a gravel-bed river that is transport-limited)
• Model:MARSSIM  + (Variable - targeted towards drainage basin or larger scales. Spatial scale determined by input parameter and run-time specification of array dimentions. Uses rectangular grid cells.)
• Model:Bing  + (Vertical resolution typically centimeters)
• Model:Compact  + (Vertical resolution typically meters)
• Model:BITM  + (Vertically: cm to m, Horizontally: 50 m to 30 km)
• Model:Sedflux  + (Vertically: mm to cm; Horizontally: 10s of m to 1000 of m)
• Model:Drainage Density  + (Very little constraint; runs quickly on large grids.)
• Model:FluidMud  + (Wave-current BL, lengthscale ~1 m nearbed, grid size ~1mm; Tidal BL: lengthscale 10 m, grid size 1cm)
• Model:Equilibrium Calculator  + (We use formulations describing rivers at l … We use formulations describing rivers at large scale. Complex interactions between physical, chemical, biological and ecological processes that play a relevant role in floodplain construction are not accounted for, as their impacts on floodplain mass balance cannot be quantified. Model parameters should thus be interpreted as averages over a few meander bends, and over several years.few meander bends, and over several years.)
• Model:Mrip  + (With Matlab running on my desktop PC I get … With Matlab running on my desktop PC I get out of memory errors when I make the domain much bigger than it is at present (250x250). I am working to expand the model domain. I would also like to increase the resolution. (Isn't this what all modelers want to do?)(Isn't this what all modelers want to do?))
• Model:Chi analysis tools  + (With reasonable parameter values channel networks with individual channel of ~1000 nodes will take a few to 10s of minutes to analyse. The longer the channel network, the longer the analysis.)
• Model:Gvg3Dp  + (With the current version of the code (DNS and no turbulence model) we are restricted to low Reynolds numbers. Up to maximum 10,000.)
• Model:Spbgc  + (With the current version of the code (DNS and no turbulence model) we are restricted to low Reynolds numbers. Up to maximum 10,000.)
• Model:TreeThrow  + (Zero dimensional model simulating a 1/12 ha plot.)
• Model:WILSIM  + (arbitrary)
• Model:Badlands  + (catchment to continental scale)
• Model:Bifurcation  + (cell size of the upstream two cells is an intrinsic model parameter, but downstream cell size can be chosen arbitrarily)
• Model:Zscape  + (described on project webpage)
• Model:TwoPhaseEulerSedFoam  + (domain needs to be large enough to capture the boundary layer, and the resolution ( on the order of grain size) should be fine enough to capture the sediment-fluid interaction near the bed level.)
• Model:Gospl  + (global scale (5 to 100 km). gospl can be u … global scale (5 to 100 km). gospl can be used with different mesh resolutions enabling better representation of surface processes in regions of interest (e.g., specific basins, continental regions) while using lower resolutions to save memory allocation in other parts (deep marine regions for example).r parts (deep marine regions for example).)
• Model:Gc2d  + (kilometers)
• Model:Plume  + (kilometers to tens of kilometers; resolution typically 10 to 100s of meters)
• Model:Dionisos  + (length : 10s - 100s of kilometers resolution : 1 km)
• Model:Wetland3P  + (length scale resolved 1-10 m)
• Model:CrevasseFlow  + (length scale: meters resolution constraint: centimeter)