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List of results

• Model:WDUNE  + (Aeolian transport and dune formation.)
• Model:CMIP  + (Air surface temperature as simulated from coupled atmosphere-ocean global climate models)
• Model:Alpine3D  + (Alpine3D is a model for high resolution si … Alpine3D is a model for high resolution simulation of alpine surface processes, in particular snow processes. The model can be driven by measurements from automatic weather stations or by meteorological model outputs. The core three-dimensional Alpine3D modules consist of a radiation balance model (which uses a view factor approach and includes shortwave scattering and longwave emission from terrain and tall vegetation) and a drifting snow model solving a diffusion equation for suspended snow and a saltation transport equation. The processes in the atmosphere are thus treated in three dimensions and coupled to a distributed one dimensional model of vegetation, snow and soil model (Snowpack) using the assumption that lateral exchange is small in these media. lateral exchange is small in these media.)
• Model:Princeton Ocean Model (POM)  + (Any 3D ocean circulation, mixing, dispersion processes, etc)
• Model:TURBINS  + (Any density driven current including particle-laden flows produced by the lock-exchange (or continuous inflow) can be simulated. The flow can interact with any arbitrary topography on the bottom.)
• Model:Gvg3Dp  + (Any type of turbidity (or gravity) currents could be modeled with this code. Is also handles the flows passing complex topographies, inflow/outflows too.)
• Model:Spbgc  + (Any type of turbidity (or gravity) currents could be modeled with this code. I also use it for modeling internal bores.)
• Model:CrevasseFlow  + (As a crevasse splay evolves, the slope of … As a crevasse splay evolves, the slope of its outflow should be no less than the slope of lower channel; and the bottom elevation of a crevasse splay should be no lower than the elevation of lowest point of channel bed, so the bottom elevation of the lowest point that a crevasse splay is able to cut down is max(hs, Zcsb).</br></br>A ratio of Q above the bottom of crevasse splay can be distributed to outflow of crevasse splay. After flow parameters for the outflow of crevasse splay are calculated, the erosion (deposition) rate of crevasse splay can be calculated, thus the morphology of crevasse splay can be updated. </br></br>When the crevasse splay has not yet cut down to the lowest point max(hs,Zcsb), it can be both widened and deepened. When the crevasse splay has cut down to the lowest point max(hs,Zcsb), it can only be widened or silted vertically. can only be widened or silted vertically.)
• Model:Landlab  + (As of autumn 2013, the library of process … As of autumn 2013, the library of process components includes the following:</br></br>- diffusion (for conductive heat transport, soil transport over terrain, or other applications of diffusion theory)</br>- single-direction flow routing over topography</br>- detachment-limited stream erosion</br>- solar radiation input as a function of topography, latitude, and time</br>- evapotranspiration</br>- soil-moisture dynamics</br>- stochastic storm generation</br>- stochastic wildfire generation</br>- impact cratering</br>- overland flow / flood inundationatering - overland flow / flood inundation)
• Model:BITM  + (BIT Model takes into consideration five di … BIT Model takes into consideration five different processes:</br>* reworking of the beach profile. The model assumes that the wave action reworks the beach profile towards an equilibrium configuration described by the Dean's equation;</br>* inner-shelf sediment redistribution, which is the redistribution of sediments beyond the beach toe determined by the bottom shear stresses produced by wind waves;</br>* overwas, which is the erosion of sediment along the beach profile and its corresponding deposition on the top of the barrier island or in the back-barrier area. Overwash is related to storm surges produced bt extreme atmospheric events;</br>* lagoonal deposition, which is the deposition of fine sediments in the accomodation space between the barrier island and the mainland;</br>* aeolian sediment reworking, which represents the wind action on the subaerial part of the island.ction on the subaerial part of the island.)
• Model:CHILD  + (Basic processes include runoff generation, water erosion and sediment transport, and gravitational erosion and sediment transport. Depending on the application, the user can apply a vegetation-growth module, various tectonic functions, and other options.)
• 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)