Search by property

From CSDMS

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.

Search by property

A list of all pages that have property "Describe length scale and resolution" with value "No longitudinal coupling, not full Stokes". Since there have been only a few results, also nearby values are displayed.

Showing below up to 26 results starting with #1.

View (previous 50 | next 50) (20 | 50 | 100 | 250 | 500)

    

List of results

  • 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: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.)
  • 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:</br></br>* to allow SWAN to be used from laboratory conditions to shelf seas and</br>* 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'.)
Retrieved from "https://csdms.colorado.edu/wiki/Special:SearchByProperty/:Describe-20length-20scale-20and-20resolution/No-20longitudinal-20coupling,-20not-20full-20Stokes"