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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:Badlands  + (Basin and Landscape Dynamics (Badlands) is … Basin and Landscape Dynamics (Badlands) is a parallel TIN-based landscape evolution model, built to simulate topography development at various space and time scales. The model is presently capable of simulating hillslope processes (linear diffusion), fluvial incision ('modified' SPL: erosion/transport/deposition), spatially and temporally varying geodynamic (horizontal + vertical displacements) and climatic forces which can be used to simulate changes in base level, as well as effects of climate changes or sea-level fluctuations.climate changes or sea-level fluctuations.)
• Model:Coastal Landscape Transect Model (CoLT)  + (Bay, marsh, and forest evolution on a coastline. Simulates marsh edge erosion, bay depth changes with wind waves, and marsh migration into coastal forests, and the carbon processes associated with these changes.)
• Model:Sedtrans05  + (Bed boundary layer for pure current, combined current and waves, and pure waves. Transport of non-cohesive sediment. Erosion, transport and deposition of cohesive sediment.)
• Model:River Network Bed-Material Sediment  + (Bed-material sediment transport and storage on a river network.)
• Model:MARSSIM  + (Bedrock fluvial incision (shear stress or … Bedrock fluvial incision (shear stress or sediment flux dependency).</br>Mass wasting (creep and threshold-limited).</br>Bedload sediment transport & deposition in streams, fans, deltas.</br>Impact cratering, aeolian deposition, lava flows.</br>Flow routing with evaporation from depressions.low routing with evaporation from depressions.)
• Model:HyLands  + (Bedrock landslides Landslide erosion and landslide-derived sediment run-out)
• Model:OceanWaves  + (Bottom orbital velocity is calculated from … Bottom orbital velocity is calculated from surface wave conditions using linear wave theory. A spectral approach is used. If input wave data are just wave height and period, a spectrum is estimated based on those as described in Wiberg and Sherwood 2008. Several spectral representations are available, and spectra can be estimated based on wind speed if surface wave conditions are unknown.ed if surface wave conditions are unknown.)
• Model:CAM-CARMA  + (CAM treats radiative transfer, tidal forci … CAM treats radiative transfer, tidal forcing from Saturn, a planetary boundary layer and surface interaction, thermal conduction in the soil and chemistry. The CARMA part of the code does the aerosol microphysics involving emission, coagulation and sedimentation.g emission, coagulation and sedimentation.)
• Model:FwDET  + (Calculate water depth from a flood extent … Calculate water depth from a flood extent polygon (e.g. from remote sensing analysis) based on an underlying DEM.</br>Program procedure:</br>1. Flood extent polygon to polyline</br>2. Polyline to Raster - DEM extent and resolution (Env)</br>3. Con - DEM values to Raster</br>4. Focal Statistics loop</br>5. Water depth calculation - difference between Focal Statistics output and DEMce between Focal Statistics output and DEM)
• Model:SINUOUS  + (Centerline migration, Floodplain sediment, and channel profile evolution, depending upon choices in the parameter input files, as detailed in the model documentation.)
• Model:AlluvStrat  + (Channel migration and avulsion building stratigrpahy)
• Model:AR2-sinuosity  + (Channel planform geometry)
• Model:BlockLab  + (Cliff failure and retreat; hillslope evolution; river erosion; block release, transport, and weathering.)
• Model:WEPP  + (Climate generation (CLIGEN), infiltration, … Climate generation (CLIGEN), infiltration, percolation, evapotranspiration, plant growth, residue management and decomposition, runoff, hydralics of overland flow, soil detachment by raindrop impact and shallow flow (interrill), soil detachment by excess flow shear stress (rill, channel), sediment transport, sediment deposition, irrigation, winter processes (snow melt, frost, thaw), channel erosion processes, sedimentation in impoundments. processes, sedimentation in impoundments.)
• Model:Compact  + (Compaction of sediment due to overlying load)
• Model:IDA  + (Computation of drainage area, which, for a particular cell, is the sum of cells that drain through that cell.)
• Model:RCPWAVE  + (Computes wave refraction and diffraction processes over an arbitrary bathymetry constrained only to have mild bottom slopes.)
• Model:Subside  + (Crustal deflection due to loading)
• Model:HexWatershed  + (DEM resampling; Depression filling; Flow direction; Flow accumulation;)
• Model:GSFLOW-GRASS  + (Discretizes a watershed into sub-catchments (for surface water) and a MODFLOW grid (for groundwater), and then uses these fundamental units to build input files for and execute GSFLOW and visualize it.)
• Model:LinearDiffuser  + (Disturbance-driven soil creep (or other processes that can be represented by 2D diffusion).)
• Model:Dionisos  + (Erosion, transport and deposition of sediments (terrestrial -> deep-marine). Carbonate production. Complex tectonics (growth faults, salt deformation).)
• Model:WAVEWATCH III ^TM  + (Evolution of wind wave spectra under influence of wind, breaking, nonlinear interactions, bottom interaction (including shoalng and refraction), currents, water level changes and ice concentrsations. No diffraction.)
• Model:BarrierBMFT  + (Explores ecogeomorphic couplings between a … Explores ecogeomorphic couplings between adjacent and non-adjacent components of the entire coastal barrier system, from the ocean shoreface to the mainland forest. Processes include: Dune growth and storm erosion; storm overwash; shoreline change (ocean and back-barrier); dynamic shoreface response to sea-level rise, overwash, and dune growth; horizontal and vertical marsh dynamics; bay depth changes with wind waves; marsh migration into coastal forests; sediment exchange between barrier-marsh-bay-forest ecosystems; and carbon processes associated with ecogeomorphic changes.ses associated with ecogeomorphic changes.)
• Model:Area-Slope Equation Calculator  + (Extract c and alpha from: Slope=cArea^alph … Extract c and alpha from:</br>Slope=cArea^alpha</br>For more details:</br>Cohen, S., G. Willgoose, and G. Hancock (2008), A methodology for calculating the spatial distribution of the area-slope equation and the hypsometric integral within a catchment, J. Geophys. Res., 113, F03027, doi:10.1029/2007JF000820.s., 113, F03027, doi:10.1029/2007JF000820.)

• Model:TauDEM  + (Flow processes that are driven by the topographic gradient)

• Model:BRaKE  + (Fluvial bedrock erosion; hillslope block delivery; block transport and degradation)
• Model:AquaTellUs  + (Fluvial erosion and depositions, lateral deposition across the floodplain, plume deposition in marine domain.)
• Model:CASCADE  + (Fluvial erosion, deposition and sedimentation, hillslope (diffusion) processes, flexure, orography)
• Model:ErosionDeposition  + (Fluvial sediment entrainment and deposition)
• Model:SPACE  + (Fluvial sediment erosion and deposition, fluvial bedrock erosion, the bedrock cover effect.)
• Model:PyDeltaRCM  + (Flux routing and sediment transport for th … Flux routing and sediment transport for the formation of river deltas. Resolves channel bifurcations, avulsion and migration. Can simulate subsidence (default basin-like shape, modify the Python code to customize). Can store stratigraphy (as sand fraction and thickness).tigraphy (as sand fraction and thickness).)
• Model:CryoGrid3  + (For forward time integration, the simplest possible scheme, first-order forward Euler, is employed.)
• Model:BOM  + (Free surface flow of water. Conservation of heat, salinity, mass, turbulent kinetic energy, dissipation.)
• Model:Symphonie  + (Free surface, generalized s coordinate model. Classical representation of oceanic processes (tides, wind circulation, density driven circulation ...). Coupling with sediment transport and biogeochemistry)
• Model:GPM  + (Free-surface flow including wave action Clastic erosion, transport, deposition Compaction (load-based, vertical porous flow, full 3D porous flow) Rudimentary carbonate growth)
• Model:GENESIS  + (GENESIS was designed to describe long-term … GENESIS was designed to describe long-term trends of the beach plan shape in the course of its approach to an equilibrium form. The shoreline change model best calculates shoreline movement in transition from one equilibrium state to another. This change is usually caused by a notable pertubation, for example, jetty construction at a harbor or inlet, or placement of beach nourishment material.r placement of beach nourishment material.)
• Model:GSFLOW  + (GSFLOW simulates flow within and among thr … GSFLOW simulates flow within and among three regions. The first region is bounded on top by the plant canopy and on the bottom by the lower limit of the soil zone; the second region consists of all streams and lakes; and the third region is the subsurface zone beneath the soil zone. PRMS is used to simulate hydrologic responses in the first region and MODFLOW-2005 is used to simulate hydrologic processes in the second and third regions.processes in the second and third regions.)
• Model:WACCM-EE  + (General circulation model of early Earth. Particular detail is paid to chemistry, RT, and haze microphysics)
• Model:Gc2d  + (Glacier growth and evolution)
• Model:GroundwaterDupuitPercolator  + (Groundwater flow and seepage)
• Model:TreeThrow  + (Growth, death, and regeneration of individual trees. Sediment flux moved by each tree.)
• Model:HSPF  + (HSPF assumes that the "Stanford Watershed … HSPF assumes that the "Stanford Watershed Model" hydrologic model is</br>appropriate for the area being modeled. Further, the instream model assumes</br>the receiving water body is well-mixed with width and depth and is thus</br>limited to well-mixed rivers and reservoirs. Application of this methodology</br>generally requires a team effort because of its comprehensive nature.ffort because of its comprehensive nature.)
• Model:Lake-Permafrost with Subsidence  + (Heat conduction in permafrost, lake ice growth-decay, permafrost subsidence due to excess ice)
• Model:MIDAS  + (Hetergeneous size-density bed and suspended load transport, evolving open channel flow)
• Model:HEBEM  + (Hydrologic processes: Precipitation, infiltration, evapotranspiration, overland flow, saturation-excess runoff, groundwater flow Geomorphic processes: Baselevel lowering, weathering, hillslope processes, erosion, sediment transport)
• Model:CAESAR Lisflood  + (Hydrology: Spatially variable TOPMODEL 2d … Hydrology: Spatially variable TOPMODEL</br>2d Hydrodynamic flow model: Using the Lisflood-FP (Bates et al., 2010) method</br>Fluvial erosion and deposition over 9 different grainsizes - through 10 active layers</br>Lateral erosion: Based on radius of curvature</br>Slope processes: Landslides and soil creep</br>Sand Dunes: Ability to couple sand dune sub model with fluvial processes.and dune sub model with fluvial processes.)
• Model:Inflow  + (Hyperpycnal flow)
• Model:Sakura  + (Hyperpycnal flow)
• Model:ILAMB  + (ILAMB takes a set of observational data en … ILAMB takes a set of observational data encoded as CF-compliant netCDF files, extracts commensurate quantities from historical model results (ideally compliant with CMOR), and then subjects them to a gauntlet of statistical measures examining aspects of performance such as bias, RMSE, phase, interannual variability, and spatial distribution. This results in a hierarchical set of webpages which display and controls the flow of information.play and controls the flow of information.)
• Model:IceFlow  + (Ice deformation, ice sliding)