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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:WEPP  + (Hillslope simulations are recommended for … Hillslope simulations are recommended for lengths not greatly exceeding 100 meters. Watershed simulations should not exceed areas above 260 hectares. Larger areas can be simulated for hillslope spatial analyses only - but the channel processes will not be accurate at these larger scales.ll not be accurate at these larger scales.)
• Model:Subside  + (Horizontal resolution is typically 100s of meters)
• Model:Inflow  + (Horizontal resolution is typically 10s of meters)
• Model:Sakura  + (Horizontal resolution is typically 10s of meters)
• Model:FVshock  + (Hundreds of Km (the reach of a river).)
• Model:HydroTrend  + (HydroTrend should be applied to river larger than 100km; and basins smaller than 75000km2.)
• Model:Pllcart3d  + (In its current state, the code is restricted to low Reynolds number and Peclet number of order 1000.)
• Model:CHILD  + (In principle, the model can address spatia … In principle, the model can address spatial scales ranging from gullies and small (~1km2) catchments to mountain ranges, as long as setup and parameters are chosen appropriately. Resolutions greater than about 10,000 nodes normally require significant computation time.ally require significant computation time.)
• Model:Quad  + (In the field, this model is applicable in the range of landscape and regional scales (~10-100km). It has also been successfully applied at the scale of physical experiments.)
• Model:IDA  + (Increasing the number of processors should allow larger/higher resolution landscapes to be considered.)

• Model:RivMAP  + (Input channel masks can be arbitrary resolution)

• Model:HexWatershed  + (It is best performance for high resolution (<100m) simulation. With the version 3.0, coarser resolution is supported through stream burning feature.)
• Model:TOPOG  + (It is intended for application to small catchments (up to 10 km2, and generally smaller than 1 km2).)
• Model:Morphodynamic gravel bed  + (It's a reach scale. It is applied to 30km downstream of the Buech river. However, if dx is changed upward/downward, the time step should be adjusted.)
• Model:CEM  + (Kilometers to hundreds of kilometers. Numerically, the model can be discretized with much smaller spatial resolution. However, the assumptions of approximately shore-parallel shoreface contours becomes unreasonable at scales smaller than kilometers.)
• Model:LISFLOOD  + (LISFLOOD is grid-based, and applications so far have employed grid cells of as little as 100 metres (for medium-sized catchments), to 5,000 metres for modelling the whole of Europe and up to 0.1° (around 10 km) for modelling on a global scale.)
• Model:CASCADE  + (Large scale (100 km+) model, suitable for orogenic scale modeling but could easily be adapted)
• Model:SPACE  + (Length scale should be reach or larger (~100m and up). Run time depends on grid size and resolution.)
• Model:ErosionDeposition  + (Length scale: ~10's of meters to ~1000's of km)
• Model:TUGS  + (Length varies, resolution is on the order of several channel width (i.e., 1D model produces only reach-averaged results).)
• Model:GNE  + (Limited by resolutn of input & river systems data; basins < 20,000 km2 currently poorly represented)