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A list of all pages that have property "Describe key physical parameters" with value "see publication". Since there have been only a few results, also nearby values are displayed.

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List of results

  • Model:DECAL  + (potential sand transport rate, sediment avaliability, vegetation response characteristics)
  • Model:Mosartwmpy  + (river channel network geometry, flow direction, and flow coefficients -- Euler equations reservoir operations -- seasonal and data driven water release behavior)
  • Model:CASCADE  + (see Braun, J. and Sambridge, M., 1997. Basin Research, v. 9, pp.27-52.)
  • Model:MARM5D  + (see Cohen et al., 2009, 2010, 2014 in JGR-ES)
  • Model:GEOMBEST  + (see User's Guide and Moore et al., 2010)
  • Model:WILSIM  + (see above references)
  • Model:XBeach  + (see manual at http://xbeach.org)
  • Model:DeltaSIM  + (see references)
  • Model:SimClast  + (tba)
  • Model:MITgcm  + (too many to describe)
  • Model:SedFoam-2.0  + (two-phase Eulerian equations for sediment transport (see the user document))
  • Model:Delft3D  + (water level, velocity, temperature, saliniwater level, velocity, temperature, salinity, density, pressure, turbulent energy, wave heights & forces, roller & breaker energy, sediment fractions, bed levels, concentrations (chloride / salinity, coliform bacteria (E. Coli, faecal and total), oxygen and BOD, temperature, organic C, N, P and Si, inorganic phosphorus, ammonium, nitrate and silica, algae (diatoms, greens, bluegreens), heavy metals, PCB-153, HCB, lindane, fluoranthene and benzo(a)pyrene)53, HCB, lindane, fluoranthene and benzo(a)pyrene))
  • Model:Gospl  + (• river incision using the stream power la• river incision using the stream power law (Howard et al., 1994) based on a multiple flow direction approach and an implicit parallel implicit drainage area method (Richardson et al., 2014),</br>• inland river deposition in depressions computed using priority-flood techniques (Barnes et al., 2014),</br>• dual-lithology marine deposition at river mouth based on a diffusion algorithm (Rivenaes, 1992),</br>• hillslope processes in both marine and inland areas (Salles, 2019), and</br>• sediment compaction as stratigraphic layers geometry and properties changes (Sclater & Christie, 1980; Yuan et al., 2019).ater & Christie, 1980; Yuan et al., 2019).)