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A list of all pages that have property "Describe processes" with value "1D flexure of a continuous elastic plate". Since there have been only a few results, also nearby values are displayed.

Showing below up to 26 results starting with #1.

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List of results

  • Model:LONGPRO  + (1D gradually varied channel flow, Total sediment transport of a river at a node, mass conservation, tectonic elevation changes, settling velocity)
  • Model:STVENANT  + (1D unsteady nonlinear gradually varied flow)
  • Model:Hyper  + (2D Turbidity Current model)
  • Model:2DFLOWVEL  + (2D, nonlinear long wave equations)
  • Model:Caesar  + (2d multiple flow direction steady state fl … 2d multiple flow direction steady state flow model</br>Erosion and deposition over 9 separate grainsizes</br>Bedload and suspended load sediment transport</br>Slope processes (creep, enhanced creep and mass movement)</br>Vegetation growth</br>Aeolian transport (under development - slab dune model)port (under development - slab dune model))
  • Model:CEM  + (A continuity equation, representing the co … A continuity equation, representing the conservation of sediment in the nearshore zone, relates gradients in alongshore sediment flux to horizontal shoreline changes, given a depth over which erosion or accretion are distributed—the depth of the shoreface. This treatment embodies the assumption that cross-shore sediment fluxes across base of the shoreface are small compared to gradients in alongshore flux. However, cross-shore sediment fluxes landward of the shoreline, associated with overwash, are treated, allowing barriers to migrate and maintain elevation relative to a rising sea level. See Ashton and Murray (2006a) for a full treatment of these model dynamics.</br></br>The material underlying the shoreline and shoreface converted to mobile sediment as it is exposed by shoreline erosion. The lithology is parameterized by two quantities that can vary across the model domain: the maximum weathering rate (which occurs when the shoreface is bare of sediment) and the composition of the resulting sediment (percentage coarse enough to stay in the nearshore system. See Valvo et al. (2006) for a full explanation of how underlying geology is treated.</br></br>Where beach nourishment is deemed by the user to be occurring, if the gradients in sediment flux would cause the shoreline to erode landward of a pre-determined location, sediment is added at the rate required to prevent such shoreline change. Hard structures are treated as if the lithology has a maximum weathering rate of 0.hology has a maximum weathering rate of 0.)
  • Model:ApsimX  + (A set of biophysical modules that simulate … A set of biophysical modules that simulate biological and physical processes in farming systems.</br>A set of management modules that allow the user to specify the intended management rules that characterise the scenario being simulated and that control the simulation.simulated and that control the simulation.)
  • Model:OTIS  + (Advection, Dispersion, Inflow, and Transient Storage. First-order loss/production, sorption.)
  • Model:Nitrate Network Model  + (Advective transport and removal of nitrate and organic carbon via denitrification in lakes, wetlands, and channels.)
  • Model:Rescal-snow  + (Aeolian sediment transport (snow or sand grains), granular motion, avalanches, snowfall, time-dependent cohesion)
  • 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.)
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