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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:CoastMorpho2D  + (Spatial resolution from 1 m to 1 km Spatial extent up to hundreds of km)
• Model:HydroPy  + (Spatial resolution is determined from the auxiliary data and meteorological forcing)
• Model:MarshPondModel  + (Spatial resolution of 1 m to simulate small ponds)
• Model:Shoreline  + (Spatial resolution of coastline is typically 1 to 50 meters.)
• Model:RiverMUSE  + (Spatial scale is implicit; resolution is n/a.)
• Model:BlockLab  + (Standard LEM constraints on length scale: reach scale and above until you run out of computing power. Resolution is constrained by block size, should generally be order 1-10 m.)
• Model:MarshMorpho2D  + (Suitable for a large range of spatial resolution (0.5 m to 100 m))
• Model:SINUOUS  + (The channel centerline is represented by X,Y coordinates with about one channel=width equivalent. The floodplain evolution, if simulated, has cells of one channel-width equivalent. Length of simulated domain and floodplain size depends upon input data.)
• Model:AR2-sinuosity  + (The channel is represented by a set of linked nodes. There are no intrinsic constrains for length scale or resolution.)
• Model:TURBINS  + (The current version is a DNS code, i.e. no … The current version is a DNS code, i.e. no turbulence model is incorporated yet. </br>Hence, grid resolution should be carefully treated to resolve all the flow scales. </br>In other words, limited by the computational costs, we are restricted to low Reynolds numbers (O(1,000)-O(10,000)).low Reynolds numbers (O(1,000)-O(10,000)).)

• Model:CMIP  + (The grid is 720 wide by 360 high, thus it a half degree resolution.)

• Model:Meander Centerline Migration Model  + (The lengths are scaled by the cross section half width of the river, i.e. the lenghts are dimensionless. Thus any kind of river scenario may be potentially simulated.)
• Model:GENESIS  + (The longshore extent of the modeled reach can range from less than 1 mile to 10's of miles.)
• Model:Tracer dispersion calculator  + (The model domain must be at least 10s of particle step length long.)
• Model:AquaTellUs  + (The model domain starts in the fluvial floodplain, the main river channel is considered an incoming boundary condition. Gridcells are typically averaged over 100's meters to 1000's of meters. Tests ran with grids of 150 by 150 km.)
• Model:PyDeCe  + (The model grid spacing is limited by the resolution of the input topography dataset.)
• 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.)