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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:CSt ASMITA  + (Time- and length-averaged sediment transport in shelf, shoreface and surf zone environments combined with morphodynamic-driven sediment flux through inlet, along ebb tide delta and with the bay or estuar.)
• Model:QDSSM  + (Time-averaged sediment transport by long-r … Time-averaged sediment transport by long-range river transport based on discharge and gradient and on short range diffusive transport based on gradient and diffusion coefficients. Thresholds for slope and discharge can be set and act as a means to keep the flow from spreading over every adjacent grid cell allowing avulsion and bifurcation processes to be modeled.n and bifurcation processes to be modeled.)
• Model:ADCIRC  + (To many to list, see http://adcirc.org)
• Model:WRF  + (To simulate real weather and to do simulat … To simulate real weather and to do simulations with coarse resolutions, a minimum set of physics components is required, namely radiation, boundary layer and land-surface parameterization, convective parameterization, subgrid eddy diffusion, and microphysics. Since the model is developed for both research and operational groups, sophisticated physics schemes and simple physics schemes are needed in the model. The objectives of the WRF physics development are to implement a basic set of physics into the WRF model and to design a user friendly physics interface. Since the WRF model is targeted at resolutions of 1-10 km, some of physics schemes might not work properly in this high resolution (e.g. cumulus parameterization). However, at this early stage of model development, only existing physics schemes are implemented, and most of them are taken from current mesoscale and cloud models. In the future, new physics schemes designed for resolutions of 1-10 km should be developed and implemented. See http://www.mmm.ucar.edu/wrf/users/docs/wrf-phy.html#physics_scheme for more informationy.html#physics_scheme for more information)
• Model:SWAT  + (Too many to describe, see: http://www.brc.tamus.edu/swat/index.html)
• Model:DeltaClassification  + (Tool is used to regionalize a study area i … Tool is used to regionalize a study area into zones with 'common physical characteristics' with the underlying aim of differentiating areas of influence of various physical processes. Regionalization attempts to aggregate spatial units or observations into clusters based on spatial continuity as well as attribute similarity. </br>Geometry metrics are derived from satellite data analysis and include a.o. island area, island aspect ratio, island fractal dimension, and surrounding channel metric, channel width, channel sinousity, number of outflow channels, convexity.ty, number of outflow channels, convexity.)
• Model:CosmoLand  + (Tracking of cosmogenic nuclides on surface and in fluvial system of a landslide dominated drainage basin)
• Model:GRLP  + (Transport-limited equilibrium-width long-profile evolution)
• Model:Cliffs  + (Tsunami propagation from a source earthquake to a coastal site, land inundation.)
• Model:LOGDIST  + (Turbulent open channel flow along a rough wall)
• Model:GeoClaw  + (Two-dimensional depth-averaged flows, particularly suitable for tsunami and storm surge modeling, and has also bee used for dam breaks and flooding of river valleys.)
• Model:Non Local Means Filtering  + (Uses a non-local means filter image processing technique to perform filtering/smoothing of a DEM.)
• Model:NEXRAD-extract  + (Uses the Python NetCDF toolkit (see python-netcdf on apt) to pull the desired information out of NetCDF files generated from NEXRAD (WSR-88D) outputs)
• Model:Cross Shore Sediment Flux  + (Using energetics-based formulations for wa … Using energetics-based formulations for wave-driven sediment transport, we develop a robust methodology for estimating the morphodynamic evolution of a cross-shore sandy coastal profile. The wave-driven cross-shore</br>sediment flux depends on three components: two onshore-directed terms (wave asymmetry and wave streaming) and an offshore-directed slope term. The cross-shore sediment transport formulation defines a dynamic equilibrium profile and, by perturbing about this steady-state profile, we present an advection-diffusion formula for profile evolution. Morphodynamic Péclet analysis suggests that the shoreface is diffusionally dominated. Using this depth-dependent characteristic diffusivity timescale, we distinguish a morphodynamic depth of closure for a given time envelope. Even though wave-driven sediment transport can (and will) occur at deeper depths, the rate of morphologic bed changes in response to shoreline change becomes increasingly slow below this morphodynamic closure depth.ow below this morphodynamic closure depth.)
• Model:Detrital Thermochron  + (Watershed erosion)
• Model:OlaFlow  + (Wave generation, propagation, shoaling, diffraction, refraction, breaking. Nonlinear wave-wave and wave-current interaction. Surf and swash hydrodynamics.)
• Model:Quad  + (We model sedimentation in a fluvio-deltaic … We model sedimentation in a fluvio-deltaic system under base-level changes. Possible dynamics include: (1) river aggradation (i.e., a seawards migration of the alluvial-basement transition), (2) river degradation (i.e., a landwards migration of the alluvial-basement transition), (3) regression (i.e., a seawards migration of the shoreline), and (4) transgression (e.g., a landwards migration of the shoreline)., a landwards migration of the shoreline).)
• Model:Bedrock Fault Scarp  + (Weathering and erosion of bedrock on a hillslope; vertical and horizontal displacement due to earthquakes.)
• Model:CMFT  + (Wind waves are computed by wave action pro … Wind waves are computed by wave action propagation, tidal current are computed with a quasi static approximation. Bottom shaer stress, computed from a combination ot the two, induces bottom erosion. Suspended sediment are advected / diffused by tidal current, and eventually sedimented back. A different erosional process are used where waves break on a vertical obstacle (the vertical scarp at the marsh boundary). Vegetation is computed as a function of the ground elevation respect to the mean tidal level. Vegetation change bottom erodability and the sediment trapping.tom erodability and the sediment trapping.)
• Model:STORM  + (cyclone winds)
• Model:Zscape  + (described on project webpage)
• Model:DECAL  + (development of dune landscapes under the interaction between aeolian sand transport and vegetation growth and response)
• Model:Delft3D  + (drying/flooding, turbulence and large eddi … drying/flooding, turbulence and large eddies, stratification, internal waves, density effects of salinity, temperature and sediment, free surface flow, wave-current interaction, wind forcing, precipitation and evaporation, sediment sorting, fluid mud, morphological change, biochemical reactions, algae modelling, nutrient cycling, atmosphere-water exchange, adsorption and desorption of substances, deposition and re-suspension of particles and adsorbed substances, bacterial , predationadsorbed substances, bacterial , predation)
• Model:FineSed3D  + (fine sediment transport in the bottom boundary layer)
• Model:SIMSAFADIM  + (fluid flow (2D potential flow), clastic sediment transport and deposition, carbonate deposition and transport, evaporate deposition, sea level change and coastline movement)

• Model:TURB  + (fluid turbulence on a wall of given hydraulic roughness)

• Model:Gospl  + (global-scale forward models of landscape evolution, dual-lithology (coarse and fine) sediment routing and stratigraphic history forced with deforming plate tectonics, paleotopographies and paleoclimate reconstructions.)
• Model:ISSM  + (ice stress balance, ice mass transport / f … ice stress balance, ice mass transport / free surface, ice thermal (cold- and enthalpy-based), dual continuum hydrology, SHAKTI hydrology, GlaDS hydrology, ice damage mechanics, transient (time-dependent projection), grounding line dynamics, glacial isostatic adjustment (GIA), solid earth elastic response, sea-level fingerprints, positive degree day (PDD), surface energy balance (snow densification and surface mass balance calculation with the GEMB model), basal melt parameterizations (PICO/PICOP), empirical scalar tertiary anisotropy regime (ESTAR), uncertainty quantification capabilities (Dakota)ainty quantification capabilities (Dakota))
• Model:DeltaSIM  + (longterm 2D deltaic sedimentation and clinoform formation for fluvial dominated deltas)
• Model:ModelParameterDictionary  + (n/a)
• Model:Drainage Density  + (n/a)
• Model:RivMAP  + (n/a)
• Model:CruAKTemp  + (n/a)
• Model:SETTLE  + (non-hindered grain settling)
• Model:Bifurcation  + (quasi-normal flow (1D) downstream and transverse sediment fluxes mass conservation (Exner))
• Model:SedFoam-2.0  + (sediment transport drive by turbulent/laminar flows)
• Model:AnugaSed  + (sediment transport, vegetation drag)
• Model:GEOMBEST  + (see User's Guide and Moore et al., 2010)
• Model:WBMsed  + (see: Sagy Cohen, Albert J. Kettner, James P.M. Syvitski, Balazs M. Fekete, WBMsed, a distributed global-scale riverine sediment flux model: Model description and validation, Computers and Geosciences, ISSN 0098-3004, 10.1016/j.cageo.2011.08.011.)
• Model:XBeach  + (short wave propagation, infragravity waves, shear waves, swash, overtopping, overwashing, breaching, longshore current, cross-shore current, suspended sediment transport, morphological changes, dune erosion)
• Model:HydroPy  + (snowmelt process, skin and canopy processes, soil processes, surface water and shallow groundwater processes, river routing)
• Model:Sedflux  + (surface plumes, hyperpycnal plumes, sediment slope failure that results in turbidity currents or debris flows, subsidence, compaction, sediment remobilization due to waves and currents, river avulsion)
• Model:TAo  + (tAo is an open-source software designed to … tAo is an open-source software designed to model the interplay between lithosphere flexure and surface transport (erosion/sedimentation), particularly during the formation of orogens and foreland sedimentary basins (see details). This 2D (cross-section) numerical model calculates 1D lithospheric flexure with different rheologies, in combination with fault kinematics, other isostatic loads, and erosion/deposition. Erosion models include both constant-rate and climate-based approaches. The programs are developed in C for Linux platforms, graphic output is produced using GMT scripts, and standard PCs match the CPU and memory requirements. The software is available under a GPL license.software is available under a GPL license.)
• Model:MITgcm  + (too many to describe)
• Model:YANGs  + (total sediment load transport)
• Model:WACCM-CARMA  + (virtually all earth atmospheric processes)
• Model:WINDSEA  + (water surface wave genesis)
• Model:Mosartwmpy  + (water volume flux, water supply, reservoir operations)
• Model:WAVEREF  + (wave refraction)
• Model:FluidMud  + (wave-current boundary layer and fluid mud transport. dilute suspension. wave-supported gravity-driven mudflow. turbulence modulation due to sediment. tidal-driven fluid mud transport. Floc dynamics. Rheology.)