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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: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).)
Model:GNE + (Limited by resolutn of input & river systems data; basins < 20,000 km2 currently poorly represented)
Model:DeltaClassification + (Methods has been applied to data set of 100's of individual delta islands derived from Landsat satellite data (30-60m resolution).)
Model:Icepack + (Minimum ~50m in x, maximum hundreds of kilometers)
Model:FuzzyReef + (Model does not place any spatial constraints.)
Model:River Temperature Model + (Model is 1D, we have used it over a x-section of a floodplain with varying flood inundation depth and durations.)
Model:DeltaSIM + (Model is intended to generate stratigraphy for 2D profiles of large deltas (100's of km's))

Model:Princeton Ocean Model (POM) + (Model used for grid size ranging from ~1m to 1000km)

Model:1D Hillslope MCMC + (Model uses a fixed hillslope length of 30 m constrained from topographic measurements.)
Model:Lake-Permafrost with Subsidence + (Near surface, length scale should be 5-10 cm if subsidence occurring. Deeper in permafrost, 1+ m okay.)
Model:NearCoM + (Nearshore regions from shoreline to 10 meter water depth. Model resolution depends on specific modules.)
Model:SNAC + (No inherent length scale or resolution as long as the continuum hypothesis is satisfied. A practical constraint on length scale and resolution is computational cost.)
Model:CarboCAT + (No intrinsic constraints)
Model:IceFlow + (No longitudinal coupling, not full Stokes)
Model:MARSSIM V4 + (None except elapsed time and memory limits.)
Model:Demeter + (Output is typically in a 0.05degree resolution)
Model:Marsh column model + (Point on marsh surface, depth of modeled column can extend to 10s of meters. Sub cm vertical resolution.)
Model:TopoFlow + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Channels-Diffusive Wave + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Channels-Dynamic Wave + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Channels-Kinematic Wave + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Diversions + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Infiltration-Green-Ampt + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Infiltration-Smith-Parlange + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Meteorology + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Snowmelt-Degree-Day + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Snowmelt-Energy Balance + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Saturated Zone-Darcy Layers + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Evaporation-Read File + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Evaporation-Energy Balance + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Evaporation-Priestley Taylor + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:TopoFlow-Infiltration-Richards 1D + (Recommended grid cell size is around 100 meters, but can be parameterized to run with a wide range of grid cell sizes. DEM grid dimensions are typically less than 1000 columns by 1000 rows.)
Model:Hilltop and hillslope morphology extraction + (Requires high resolution (1 m LiDAR) topographic data.)