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: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. </br></br>Reference</br>Lauer, 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)
• Model:CVPM  + (no known constraints)
• Model:TopoToolbox  + (none)
• Model:Bifurcation  + (none)
• Model:Barrier Inlet Environment (BRIE) Model  + (sea-level rise timescales (decades to millennia). Parameterizations not suitable for short-timescale analyses)
• Model:GEOMBEST  + (see User's Guide and Moore et al., 2010)
• Model:TOPMODEL  + (see the discussion of limitations in Beven et al., 1995 and Beven, 1997. Variable, from 1 to 24 hours)
• Model:Badlands  + (thousands to millions of years)
• Model:Dionisos  + (time scale : 10s of ky - 100s of My resolution : some kyr.)
• Model:CrevasseFlow  + (time scale: decades resolution constraints: day)
• Model:FineSed3D  + (time step should be small enough to ensure the CFL criterion.)
• Model:Wetland3P  + (time step ~ 1-100 days do not resolve tides)
• Model:WACCM-CARMA  + (typically 30-minute time steps)
• Model:XBeach  + (typically used on storm timescale; will be extended to cover up to years)
• Model:Kudryavtsev Model  + (yearly)
• Model:OlaFlow  + (~10 minutes to weeks)