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A list of all pages that have property "Describe key physical parameters" with value "See documentation and published papers using MARSSIM". Since there have been only a few results, also nearby values are displayed.

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List of results

  • Model:BlockLab  + (River and hillslope erosion coefficients, hillslope weathering parameters; initial block size, block release/motion thresholds, block weathering rate.)
  • Model:SUSP  + (Rouse Equation)
  • Model:SWAN  + (SWAN contains a number of physical process … SWAN contains a number of physical processes (see Scientific/Technical documentation) that add or withdraw wave energy to or from the wave field. The processes included are: wind input, whitecapping, bottom friction, depth-induced wave breaking, obstacle transmission, nonlinear wave-wave interactions (quadruplets and triads) and wave-induced set-up. SWAN can run in several modes, indicating the level of parameterization. SWAN can operate in first-, second- and third-generation mode. The first- and second-generation modes are essentially those of Holthuijsen and De Boer (1988); first-generation with a constant Phillips "constant" of 0.0081 and second-generation with a variable Phillips "constant". An overview of the options is given in Table below.ew of the options is given in Table below.)
  • Model:SWMM  + (SWMM conceptualizes a drainage system as a … SWMM conceptualizes a drainage system as a series of water and material flows between several major environmental compartments. These compartments and the SWMM objects they contain include:</br></br>* The Atmosphere compartment, from which precipitation falls and pollutants are deposited onto the land surface compartment. SWMM uses Rain Gage objects to </br>represent rainfall inputs to the system.</br>* The Land Surface compartment, which is represented through one or more Subcatchment objects. It receives precipitation from the Atmospheric compartment in the form of rain or snow; it sends outflow in the form of infiltration to the Groundwater compartment and also as surface runoff and pollutant loadings to the Transport compartment. </br>* The Groundwater compartment receives infiltration from the Land Surface compartment and transfers a portion of this inflow to the Transport compartment. This compartment is modeled using Aquifer objects. </br>* The Transport compartment contains a network of conveyance elements (channels, pipes, pumps, and regulators) and storage/treatment units that transport water to outfalls or to treatment facilities. Inflows to this compartment can come from surface runoff, groundwater interflow, sanitary dry weather flow, or from user-defined hydrographs. The components of the Transport compartment are modeled with Node and Link objects.</br></br>Not all compartments need appear in a particular SWMM model. For example, one could model just the transport compartment, using pre-defined hydrographs as inputs., using pre-defined hydrographs as inputs.)
  • Model:Non Local Means Filtering  + (Search window radius: The distance around … Search window radius: The distance around each cell over which to evaluate the non-local mean.</br>Similarity Window Radius: The distance around each cell in the neighbourhood over which to evaluate the mean.</br>Degree of filtering: The weighting for the gaussian kernel controlling the strength of filtering and therefore the decay of weights as a function of distance from the centre of the kernel.of distance from the centre of the kernel.)
  • Model:CoastMorpho2D  + (See -G Mariotti, S Murshid, 2018, A 2D Tid … See</br>-G Mariotti, S Murshid, 2018, A 2D Tide-Averaged Model for the Long-Term Evolution of an Idealized Tidal Basin-Inlet-Delta System, Journal of Marine Science and Engineering 6 (4), 154</br>-G Mariotti, 2020, Beyond marsh drowning: The many faces of marsh loss (and gain)</br>Advances in Water Resources, 103710 gain) Advances in Water Resources, 103710)
  • 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'.)
  • Model:Rescal-snow  + (See 'rescal_snow_input' in docs.)
  • Model:Cyclopath  + (See Burgess et al. (2001), Basin Research)
  • Model:TUGS  + (See Cui (2007a) for detail: http://dx.doi.org/10.1029/2006WR005330)
  • Model:ErosionDeposition  + (See Davy and Lague (2009, Journal of Geophysical Research) for full model description.)
  • Model:Sakura  + (See Kubo 2003 (doi:10.1016/j.sedgeo.2003.11.002))
  • Model:RASCAL  + (See Larsen and Harvey, 2010, Geomorphology and Larsen and Harvey, 2010, American Naturalist (currently in press))
  • Model:SBEACH  + (See SBEACH documentation (http://chl.erdc.usace.army.mil/chl.aspx?p=s&a=Software;31 ).)
  • Model:Inflow  + (See Skene et al., 1997 (doi:10.1016/S0098-3004(97)00064-2))
  • Model:TURB  + (See Slingerland et al. (1994))
  • Model:LITHFLEX1  + (See Slingerland et al. (1994))
  • Model:LITHFLEX2  + (See Slingerland et al. (1994))
  • Model:FLDTA  + (See Slingerland et al. (1994) and Henderson (1966))
  • Model:WRF-Hydro  + (See WRF-Hydro Technical Description https://ral.ucar.edu/projects/wrf_hydro/technical-description-user-guide)
  • Model:OceanWaves  + (See Wiberg and Sherwood 2008, Computers & Geosciences 34: 1243-1262 for key equations.)
  • Model:GRLP  + (See Wickert and Schildgen, 2018, Equations 20 and 36)
  • Model:OTTER  + (See Yanites 2018, JGR)
  • Model:FuzzyReef  + (See above)
  • Model:EstuarineMorphologyEstimator  + (See article: https://doi.org/10.3390/rs10121915)
  • Model:Landlab  + (See documentation at: http://landlab.readthedocs.org)
  • Model:ISSM  + (See https://issm.jpl.nasa.gov/)
  • Model:TIN-based Real-time Integrated Basin Simulator (tRIBS)  + (See https://tribshms.readthedocs.io/en/latest/)
  • Model:FUNWAVE  + (See manual)
  • Model:SPHYSICS  + (See manual)
  • Model:REF-DIF  + (See manual version3)
  • Model:STWAVE  + (See manual, is uploaded)
  • Model:Glimmer-CISM  + (See paper)
  • Model:Nitrate Network Model  + (See readme file with the source file download or related publication by J. A. Czuba.)
  • Model:River Network Bed-Material Sediment  + (See readme file with the source file download or related publications by J. A. Czuba.)
  • Model:AquaTellUs  + (See references.)
  • Model:RiverMUSE  + (See the associated published paper: https://doi.org/10.1086/684223 and the readme file for parameter descriptions.)
  • Model:TOPOG  + (See website, too many to describe: http://www-data.wron.csiro.au/topog/)
  • Model:HydroTrend  + (See: *Kettner, A.J., and Syvitski, J.P.M., … See:</br>*Kettner, A.J., and Syvitski, J.P.M., 2008. HydroTrend version 3.0: a Climate-Driven Hydrological Transport Model that Simulates Discharge and Sediment Load leaving a River System. Computers & Geosciences, Special Issue.</br>More details about the long term sediment routine that is incorporated in the Hydrotrend:</br>*Syvitski, J.P.M., Milliman, J.D., 2007. Geology, 115, 1-19..M., Milliman, J.D., 2007. Geology, 115, 1-19.)
  • Model:FwDET  + (See: Version 2.0: Cohen et al. (2019), The … See:</br>Version 2.0: Cohen et al. (2019), The Floodwater Depth Estimation Tool (FwDET v2.0) for Improved Remote Sensing Analysis of Coastal Flooding. Natural Hazards and Earth System Sciences (NHESS)</br> </br>Version 1.0: Cohen, S., G. R. Brakenridge, A. Kettner, B. Bates, J. Nelson, R. McDonald, Y. Huang, D. Munasinghe, and J. Zhang (2017), Estimating Floodwater Depths from Flood Inundation Maps and Topography. Journal of the American Water Resources Association (JAWRA):1–12. Water Resources Association (JAWRA):1–12.)
  • Model:1DBreachingTurbidityCurrent  + (See: Eke, E., Viparelli, E., and Parker, G., 2011. Field-scale numerical modeling of breaching as a mechanism for generating continuous turbidity currents. Geosphere, 7, 1063-1076. Doi: 10.1130/GES00607.1)
  • Model:Cliffs  + (Shallow-water equations)
  • Model:GPM  + (Shallow-water equations for fluid flow Separate equations for wave propagation Shield's criterion and transport capacity criterion for clastic transport (similar to SEDSIM) Sigle-phase flow in porous media for vertical and 3D compaction options.)
  • Model:BRaKE  + (Shear stress-driven fluvial erosion, primarily modulated by bed erodibility, critical bed shear stress, block delivery, and block size.)
  • Model:Alpine3D  + (Snow settling, temperature diffusion, snow saltation and suspension, snow metamorphism, terrain radiation.)
  • Model:DepthDependentDiffuser  + (Soil flux is calculated at the product of diffusivity, a characteristic transport depth, and an exponential velocity profile based on total soil depth.)
  • Model:2DFLOWVEL  + (Solves the non-linear, depth-averaged conservation equations, using finite difference scheme of Koutitas (1988))
  • Model:TreeThrow  + (Species specific, logistic growth equation for individual trees. Sediment flux for each tree fall a function of sediment volume, transport distance, and hillslope angle. Sediment volume and transport distance a function of tree diamter.)
  • Model:WAVEWATCH III ^TM  + (Spectral action balance equation.)
  • Model:IncrementalDebrisFlowVolumeAnalyzer  + (Standard flow routing and uniform sampling principles are used to govern the processes of this model.)
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