Search by property

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:CMIP  + (Data covers 1901 to 2100. It is processed from the original data to comprise a monthly timescale.)
• Model:Sedflux  + (Days or greater. Component processes can have much higher resolutions for numerical stability.)
• Model:FVshock  + (Days/months. When running for more then few month the simulation time is very large.)
• Model:Demeter  + (Decades to centuries)
• Model:RivMAP  + (Dependent on resolution and extent of input imagery)
• Model:GSSHA  + (Dependent upon computational power and memory.)
• Model:Landlab  + (Depends on application/process)
• Model:ParFlow  + (Depends upon application.)
• Model:GOLEM  + (Designed for time scales over which topography changes appreciably, which might be years for badlands, up to thousands or millions of years for other landscapes.)
• Model:AquaTellUs  + (Developed as a stratigraphic model, approach is event-based. Intended time scale ranges from several decades to Holocene (10-10.000yrs).)
• Model:TopoFlow  + (Each process can have its own timestep. Typical timesteps are: *Channel flow (seconds) *Infiltration (seconds to minutes) *Snowmelt (hours to days) *Subsurface flow (hours to days), etc. Model can be run for a full year or longer, if necessary.)
• Model:CASCADE  + (Evolution of Myrs, due to the model parameterization used (no human-scale proceses))
• Model:Bing  + (For stability, time step is typically fractions of a second)
• Model:TUGS  + (For typical application in a natural river as a prediction tool, the recommended resolution is annual, although it can be as high as hours for simulation of a specific known event.)
• Model:GPM  + (From seconds to about 100,000 years.)
• Model:GENESIS  + (GENESIS is a long-term shoreline evolution model and is best applied to estimate shoreline change over time periods of 1 year to 10's of years.)
• Model:MarshMorpho2D  + (Generally runs with very large time steps (1 year) Cannot resolve intra-tidal processes (i.e., ebb-flood variability))
• Model:NearCoM  + (Hours to months.)
• Model:ROMS  + (Hours, days, seasons. It also can be used for climate research (decades).)
• Model:ChesROMS  + (Hours, days, seasons. It also can be used for climate research (decades).)
• Model:CBOFS2  + (Hours, days, seasons. It also can be used for climate research (decades).)
• Model:UMCESroms  + (Hours, days, seasons. It also can be used for climate research (decades).)
• Model:CAM-CARMA  + (I am running the model with dynamical time steps of 1800 seconds, but it only computes the radiative transfer every 200 timesteps.)
• Model:Cyclopath  + (Internal time step years to decades Model chron resolution 1000 years Total run time 1-10 My)
• Model:AnugaSed  + (Internal timestep is determined by ANUGA for numerical stability (in seconds). Output timestep is set by the user. Simulations are realistically limited to a few model hours.)

• Model:Morphodynamic gravel bed  + (It is applied for 90 years. The time step is ~0.7 days.)

• Model:GullyErosionProfiler1D  + (It is typically run for times no less than 25 years and no greater than 700 years.)
• Model:WBMsed  + (It simulate at daily time-steps. Maximum available datasets time-span is between 1901-present.)
• Model:River Network Bed-Material Sediment  + (Limited by computational resources.)
• Model:Nitrate Network Model  + (Limited by computational resources.)
• Model:LISFLOOD  + (Long-term water balance can be simulated (using a daily time step), as can individual flood events (using hourly time intervals, or even smaller). The output of a “water balance run” can be used to provide the initial conditions of a “flood run”.)
• Model:GRLP  + (Longer than the intermittency between channel-forming events)
• Model:DeltaClassification  + (Mapview at a given time)
• Model:BITM  + (Millennial scale)
• Model:HydroTrend  + (Minimal runtime: 1yr; up to > 10kyrs Daily discharge is the smallest output timestep)
• Model:RiverMUSE  + (Model constructed for daily time steps, but can be altered with little effort.)
• Model:Lake-Permafrost with Subsidence  + (Model needs daily (or smaller) timesteps.)
• Model:CoastMorpho2D  + (Morphological time steps can be on the order of years Time steps shorter than one tidal period are not realistic)
• Model:GEOtop  + (Most forcings are required at hourly scale. Integration time step is what required by numerical algorithms to converge (depends actually on processes))
• Model:DeltaSIM  + (Mostly tested for Holocene applications (>10,000yrs), potentially longer time scales.)
• Model:Non Local Means Filtering  + (N/A)
• Model:BOM  + (No assimilation means it works best for simulations shorter than ~6months unless boundary conditions are carefully tuned to avoid model drift.)
• Model:DrEICH algorithm  + (No time resolution constraints as this software performs topographic analysis.)
• Model:SurfaceRoughness  + (No time resolution constraints as this software performs topographic analysis.)
• Model:Hilltop flow routing  + (No time resolution constraints as this software performs topographic analysis.)
• Model:HexWatershed  + (None)
• Model:MARSSIM V4  + (None except elapsed time and memory limits.)
• Model:AR2-sinuosity  + (Not applicable - the model generates static channel planforms.)
• Model:Mrip  + (One second has been the time resolution. I haven't played with this.)
• Model:GNE  + (Operates at annual scale; monthly-seasonal time steps are being explored.)
• Model:NEXRAD-extract  + (Radar sweeps every approx. 15 minutes)