Search by property

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: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)