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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: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.)
Model:GEOtop + (Resolution is limited by RAM. Processes however are parametrized at a few square meter scale.)
Model:Bedrock Fault Scarp + (Resolution on order of one to a few meters. Domain length grows over time, reaching order tens to hundreds of meters long.)
Model:SBEACH + (SBEACH is a beach profile evolution model. The model domain should extend from the landward limit of wave run-up offshore to the depth of closure.)
Model:SWAN + (SWAN can be used on any scale relevant for … SWAN can be used on any scale relevant for wind generated surface gravity waves. However, SWAN is specifically designed for coastal applications that should actually not require such flexibility in scale. The reasons for providing SWAN with such flexibility are:* to allow SWAN to be used from laboratory conditions to shelf seas and* to nest SWAN in the WAM model or the WAVEWATCH III model which are formulated in terms of spherical coordinates.mulated in terms of spherical coordinates.)
Model:OTTER + (Sediment transport models can become unstable and limit computational efficiency.)
Model:PHREEQC + (See 'Description of Input and Examples for PHREEQC Version 3 - A computer program for speciation, batch-reaction, one-dimensional transport, and inverse geochemical calculations'.)
Model:WRF-Hydro + (See WRF-Hydro Technical Description https://ral.ucar.edu/projects/wrf_hydro/technical-description-user-guide)
Model:SPHYSICS + (See manual)
Model:FwDET + (See: Version 2.0: Cohen et al. (2019), The … See:Version 2.0: Cohen et al. (2019), The Floodwater Depth Estimation Tool (FwDET v2.0) for Improved Remote Sensing Analysis of Coastal Flooding. Natural Hazards and Earth System Sciences (NHESS) Version 1.0: Cohen, S., G. R. Brakenridge, A. Kettner, B. Bates, J. Nelson, R. McDonald, Y. Huang, D. Munasinghe, and J. Zhang (2017), Estimating Floodwater Depths from Flood Inundation Maps and Topography. Journal of the American Water Resources Association (JAWRA):1–12. Water Resources Association (JAWRA):1–12.)
Model:SimClast + (SimClast can theoretically be used on a le … SimClast can theoretically be used on a length scale upwards of 20 kms, the upper limit is dependant on memory and processing restrictions. Typical length scales vary from 25 to 500 km. The highest resolution is mainly dependant on the use of intracellular fluvial deposition, as described in Dalman & Weltje (2008) this restricts the minimum cell size to 4 kms. Recent addition of floodplain process reduces this to 500 m.n of floodplain process reduces this to 500 m.)
Model:SISV + (Since we are doing DNS, we are restricted to low Reynolds numbers. Up to ~50,000 or possibly higher but very slow.)
Model:Kudryavtsev Model + (Solutions are generated for a 1D vertical column. When input data are gridded, maps of 1D vertical columns can be made.)
Model:MCPM + (Spatial resolution 0.1-1 m Cross section generally 100 m wide)
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. Hence, grid resolution should be carefully treated to resolve all the flow scales. 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.)
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:# 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.# 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.)