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A list of all pages that have property "Describe length scale and resolution" with value "Depends upon application.". Since there have been only a few results, also nearby values are displayed.

Showing below up to 26 results starting with #1.

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List of results

  • Model:SurfaceRoughness  + (A requirement is high resolution topographic data, typically ~1m resolution. For a detailed discussion of lengthscale and resolution constraints we urge the user to refer to the original manuscript)
  • Model:ESCAPE  + (A set of four examples is provided (eSCAPE-demo - https://github.com/Geodels/eSCAPE-demo) and illustrates the different capabilities of the code from synthetic to regional, to continental and to global scale models.)
  • Model:GeoClaw  + (Adaptive refinement allows using a very coarse grid on the ocean scale (e.g. 2 degree resolution) and several nested levels of refinement down to e.g. 1/3 arc-second (10 meter) resolution in specific coastal regions.)
  • Model:TopoToolbox  + (All spatial data should be provided as projected, georeferenced (e.g., UTM) grids or shapefiles where spatial units are given in meters. Data referenced in a geographic coordinate system will return unexpected results.)
  • Model:Sun fan-delta model  + (Alluvial channel morphology is not explicitly modeled; rather, channel width, depth, slope, and discharges of water and sediment are represented as sub-grid characteristics. Each cell contains at most one channel.)
  • Model:1D Particle-Based Hillslope Evolution Model  + (Although the hillslope length and height aAlthough the hillslope length and height are specified, these are dimensionless numbers from the perspective of the module. Accordingly, the resolutions supported by the module are primarily constrained by the language in which it is implemented. However, the process of "dimensionalizing" the module's outputs may place practical constraints on resolution. The associated paper discusses this issue.The associated paper discusses this issue.)
  • Model:GFlex  + (Analytical solution produces unrealistic results with low elastic thickness and/or very large cells due to the Green's function approximation.)
  • Model:NEXRAD-extract  + (Angular resolution around the radar; gridded data typically have km-nmi-size pixels)
  • Model:TauDEM  + (Applies to any resolution topographic grid, though is most sensible for grids with resolution from 2 to 50 m.)
  • Model:REF-DIF  + (Assumptions: The REF/DIF 1 model, in parabAssumptions:</br>The REF/DIF 1 model, in parabolic form, has a number of assumptions inherent in it and it is necessary to discuss these directly. These assumptions are: </br># Mild bottom slope.</br># Weak nonlinearity.</br># The wave direction is confined to a sector ±70 ◦ to the principal assumed wave direction, due to the use of the minimax wide angle parabolic approximation of Kirby (1986b). parabolic approximation of Kirby (1986b).)
  • Model:GLUDM  + (At the moment the resolution of the input controls the resolution of the output. This is a global model but can be applied to smaller domains.)
  • Model:WBMsed  + (Available datasets are for global and continental domains. Realistic high-res simulations for global scale is 6 arc-min and for continental 3 arc-min. Higher resolution datasets are available for both (e.g. 15 arc-sec for Europe).)
  • Model:GEOMBEST++  + (Cell length - 10 - 100 meters Cell height - 0.01 - 0.5 meters)
  • Model:GEOMBEST++Seagrass  + (Cell length: 10 - 100 m (typically 50 m) Cell height 0.01 - 0.5 m (typically (0.1 m))
  • Model:CarboLOT  + (Cells are approximately 1-1000m in scale; map areas 10-100km on side.)
  • Model:Barrier Inlet Environment (BRIE) Model  + (Coastal barrier ~10-100 km length scales, and ~100 m alongshore resolution. Parameterizations not suitable for small-scale (tidal inlet etc) analyses)
  • Model:RASCAL  + (Code has been most commonly run for 10x5 mCode has been most commonly run for 10x5 m cells (with the long axis parallel to flow) and domain size of 1.27 x 1.86 km. Other scales are possible, but adding additional cells will slow down processing. This model is only designed to simulate mean flows; resolution of fine turbulence structure is not possible with the code.e structure is not possible with the code.)
  • Model:Area-Slope Equation Calculator  + (Computer memory.)
  • Model:GEOMBEST-Plus  + (Constraints: * Cell length - 10 - 100 meters * Cell height - 0.01 - 0.5 meters)
  • Model:BarrierBMFT  + (Cross-shore transect length can extend 10's of km from the ocean barrier shoreface into the mainland. Grid resolution on the barrier is 10 m, and 1 m spacing from the back-barrier marsh to the mainland.)
  • Model:CAM-CARMA  + (Currently there are only initial data sets for 10x15 degrees longitude and latitude. This model is meant for global scale dynamics.)
  • Model:WACCM-EE  + (Currently, 4x5 degree, with 66 vertical levels up to 140 km. Resolution can be increased if neccessary)
  • Model:Avulsion  + (Delta-scale)
  • Model:GSSHA  + (Dependent upon computational power and memory.)
  • Model:Landlab  + (Depends on application/process)
  • Model:PyDeltaRCM  + (Domain should be 10s of Kms in x and y. Cell spacing should be 10s of meters.)
  • Model:FineSed3D  + (Domain should be large enough to resolve the bottom boundary layer, meanwhile, the grid resolution should be fine enough to resolve all the essential turbulence scales.)
  • Model:Kirwan marsh model  + (Domain size is 3 km by 3 km, grid cell is 5 m by 5m.)
  • Model:CruAKTemp  + (Downsampled from original data to 10 km by 10 km resolution)
  • Model:CosmoLand  + (Drainage basin size controls the length of the model runs. Cell size should not be increased to shorten model runs.)
  • Model:ROMS  + (Estuary, regional, and basin scales. There are couple of global applications.)
  • Model:ChesROMS  + (Estuary, regional, and basin scales. There are couple of global applications.)
  • Model:CBOFS2  + (Estuary, regional, and basin scales. There are couple of global applications.)
  • Model:UMCESroms  + (Estuary, regional, and basin scales. There are couple of global applications.)
  • Model:GPM  + (From a few hundred m to a few hundred Km)
  • Model:TAo  + (From continental to regional scale (>50 km). Up to a few thousand cells are well handled.)
  • Model:ISSM  + (From hundreds of meters to thousands of kilometers (constraints are mainly HEC-related).)
  • Model:GSFLOW-GRASS  + (GSFLOW is intended for modeling catchments from the km-scale to the 100s-of-km scale)
  • Model:Caesar  + (Has been applied to catchments ranging from 1km^2 to 500km^2, at grid resolutions ranging from 1m to 50m.)
  • Model:GOLEM  + (Has been used on scales from small (few km2) watersheds to sub-continental areas.)
  • Model:WEPP  + (Hillslope simulations are recommended for Hillslope simulations are recommended for lengths not greatly exceeding 100 meters. Watershed simulations should not exceed areas above 260 hectares. Larger areas can be simulated for hillslope spatial analyses only - but the channel processes will not be accurate at these larger scales.ll not be accurate at these larger scales.)
  • 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 spatiaIn 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.)