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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:TauDEM + (This is a static model so there is no time scale or resolution)
Model:CMFT + (Time resolution 30 min, simualtion length about 100 years.)
Model:MCPM + (Time resolution ~ 1 minute (it explicitly simulates tides))
Model:SNAC + (Time scale is essentially set by the Coura … Time scale is essentially set by the Courant condition: practially by P-wave velocity or maxwell time according to the constitutive model being considered. However, the mass scaling technique allows significantly increased time steps values from the usual dynamic one.e steps values from the usual dynamic one.)
Model:HEBEM + (Time scale of 10,000 years. Typical time step is 3 hour)
Model:WASH123D + (Time scale ranges to seconds (for example, dam break problems) to tens of years (for example real time simulations of large watersheds).)
Model:SPACE + (Time scale will be set by discharge calculation method. The model is in general intended for annual to geological time scales, but shorter time scales may be used if Landlab dynamic flow routing components are employed.)
Model:ErosionDeposition + (Time scale: Days to millions of years)
Model:Tracer dispersion calculator + (Time scales should be long compared to the … Time scales should be long compared to the time scales of short-term bed elevation changes, i.e. changes in instantaneous bed elevation associated with bedload transport and bedform migration (Blom et al., 2003, Wong et al., 2007). In other words, model results are averages over short-term bed elevation changes. For applications at field scales, the time resolution should be at least of one year because the model runs with formative conditions representative of mean annual values. REFERENCESBlom, A., Ribberink, J. S. & de Vriend, H. (2003). Vertical sorting in bed forms: Flume experiments with a natural and a trimodal sediment mixture. Water Resources Research, 39 (2), 1025.Wong, M., Parker, G., DeVries, P., Brown, T. M. & Burges, S. J. (2007). Experiments on dispersion of tracer stones under lower-regime plane-bed equilibrium bedload transport. Water Resources Research, 45, W03440.d transport. Water Resources Research, 45, W03440.)
Model:GEOMBEST++ + (Time step - 1 - 50 years Duration - Hundreds to thousands of years)
Model:HydroPy + (Time step and simulation period are determined from the auxiliary data and meteorological forcing)
Model:Cliffs + (Time step is limited by Courant stability criteria (CFL < 1). Typical time step for open-ocean propagation: 15 s; near the coast: 0.5-5 s. Typical simulation time for geophysical tsunamis: few to 36 hours.)
Model:GEOMBEST++Seagrass + (Time step: 2-50 years (typically 10 years) Duration: Centuries to millennia)
Model:BarrierBMFT + (Time step: one year, with multiple storms occurring within each year Duration: years to centuries)
Model:Barrier3D + (Time step: one year, with multiple storms occurring within each year Duration: years to millennia)
Model:GeoClaw + (Time steps are limited by CFL condition based on depth of fluid. Finer grids can automatically refine to use finer resolution in time than the underlying coarse grids.)
Model:WAVEWATCH III ^TM + (Time steps from seconds to 1h. Time length of runs can be up to years.)
Model:QDSSM + (Time steps of 10 – 1000 years depending on output range. Total range up to Millions of years.)
Model:GSFLOW-GRASS + (Time to create the model domain increases with the number of intersections between segments, catchment sub-basins, and the MODFLOW grid.)
Model:CarboLOT + (Timestepping is usually annual, extending over 1000 years. However the model is capable of doing finer and longer runs.)
Model:BlockLab + (Timesteps in the range of 1-10 years are generally stable, can run for as long as desired until the memory runs out.)
Model:Chi analysis tools + (Topographic analysis so no time scale constraints.)
Model:SimClast + (Total time scale is merely dependant on computing time, typically on the order of several thousands to 100,000 years. Time steps are restricted to 1 year.)
Model:Erode + (Typical simulated time is 1000 to 100,000 years.)
Model:Bedrock Fault Scarp + (Typical time scale of order tens to hundreds of thousands of years.)

Model:ISSM + (Typical time step of two weeks (constraints are mainly HEC-related).)

Model:TopoFlow-Evaporation-Read File + (Typical timesteps are on the order of seconds to minutes. Model can be run for a full year or longer, if necessary.)
Model:TopoFlow-Evaporation-Energy Balance + (Typical timesteps are on the order of seconds to minutes. Model can be run for a full year or longer, if necessary.)
Model:TopoFlow-Evaporation-Priestley Taylor + (Typical timesteps are on the order of seconds to minutes. Model can be run for a full year or longer, if necessary.)
Model:DynEarthSol3D + (Typically millions of years to tens of millions of year)
Model:MARSSIM + (Variable - Limited by computer speed.)
Model:FluidMud + (Wave-current BL: timescale ~10 min; time step ~0.01 sec; Tidal BL: timescale days and time step 10 s)
Model:Equilibrium Calculator + (We present an equilibrium solution that ma … We present an equilibrium solution that may or may not be reached. The fundamental assumption is that in the absence of subsidence, uplift and change of downstream water surface base level, an alluvial river will evolve toward an equilibrium state in which overbank and bar deposition (floodplain construction) are perfectly balanced by the removal of floodplain sediment due to channel migration (floodplain shaving) (Lauer & Parker, 2006). This equilibrium state can be reached if hydrologic regime, sediment supply and caliber do not vary in time. ReferenceLauer, J. W. & Parker, G. (2006). Net local removal of floodplain sediment by river meander migration, Geomorphology 96, 123-149.iver meander migration, Geomorphology 96, 123-149.)
Model:Quad + (We use the ‘basin equilibrium timescale’ (Paola 2000), defined as the length scale square divided by the fluvial diffusivity. In field settings, this time scale can range from centennial to millennia up to millions of years.)
Model:MarshPondModel + (Yearly time steps are appropriate)
Model:CosmoLand + (Yearly timesteps. Most runs go for 500,000 yrs or more.)
Model:GLUDM + (Yearly, 1960-2100.)
Model:CEM + (Years to millenia. Typically, the model is … Years to millenia. Typically, the model is run with timesteps on the order of a day. However, the assumptions that the shoreface progrades or erodes while maintaining its cross-shore shape prevents model results from being interpreted as meaningful over time scales shorter than years to decades. (Storm and post storm cross-shore shifting of sediment within the shoreface causes shoreline fluctuations on event timescales that are implicitly averaged out in this model.)re implicitly averaged out in this model.))
Model:WILSIM + (arbitrary)
Model:WOFOST + (days)
Model:Coastal Dune Model + (days- years)
Model:Mosartwmpy + (default settings represent a 3 hour time step for larger scale dynamics, and 1 hour time step for water volume flux subdivided into smaller iterations based on localized grid cell parameters (can get as small as ~12 minutes for some cells))
Model:Zscape + (described on project webpage)
Model:PIHM + (fully implicit, time adaptive, based on the CVODE ODE solver from LBL)
Model:Icepack + (inimum several days, maximum hundreds-thousands of years)
Model:Gospl + (long term (several millions of years) problems.)
Model:DECAL + (lower limit akin to days, no upper limit)
Model:Frost Model + (mean annual conditions)
Model:Delft3D + (minutes (time scales of eddies) to centuries (long-term morphology))
Model:ModelParameterDictionary + (n/a)
Model:Drainage Density + (n/a)