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No but possible  +
2798  +
Hull  +
No but possible  +
No but possible  +
United Kingdom  +
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13:07:22, 13 February 2009  +
Yes, I am happy to collaborate with any potential users. There is a long history of CAESAR being take up by others including researchers in Italy, France, Spain, NZ, Australia, USA.  +
Tested on several catchments in UK over long and short time scales.  +
none yet; in development  +
Flow and sediment discharge data, images of topographic change  +
DEM as ascii grid (output from arcGIS), Rainfall data as a space separated ascii file (straightforward list), Inputs of water/sediment in an ascii file. Other single value parameter inputs for grainsize, flow parameters, slope processes etc..  +
Flow depths calculated using version of maFlow depths calculated using version of mannings implemented across a cellular grid using a scanning algorithm.</br>Sediment tranport using either Einstein or Wilcock and Crowe functions</br>Slope model using simple slab failure and psuedo USLE implementation</br>Dune model adaption of DECAL and Werner slab modelel adaption of DECAL and Werner slab model  +
Has been applied to catchments ranging from 1km^2 to 500km^2, at grid resolutions ranging from 1m to 50m.  +
Run times can be long (60 +days for large areas over many 100's of years). Flow model is steady state  +
ascii grids (readable into arcGIS) and gooascii grids (readable into arcGIS) and google earth images of: DEM, flow depth, surface grainsize, shear stress, vegetation cover, velocity.</br>Also time series of water discharge and sediment discharge (across 9 grainsizes) at user chosen interval.</br>Also visual output to AVI file. interval. Also visual output to AVI file.  +
2d multiple flow direction steady state fl2d 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)  +
The model has simulated periods from 1 dayThe model has simulated periods from 1 day to 9000 years.</br>The length of run is largely contingent on the number of grid cells, thus a balance between resoltion and area of study. A small catchment with a coarse resolution will run very fast. Increase the area or make grid cells smaller and run times will increase.cells smaller and run times will increase.  +
CAESAR is a cellular landscape evolution model, with an emphasis on fluvial processes, including flow routing, multi grainsize sediment transport. It models morphological change in river catchments.  +
Tom  +
29  +
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University of Hull  +
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Coulthard  +
1.16  +
Terrestrial  +
cellular  +, model  +, including flow routing  +, multi grainsize sediment  +, grainsize sediment transport  +, cellular landscape evolution  +, landscape evolution model  +, fluvial processes  +, including flow  +, flow routing  +, multi grainsize  +, sediment transport  +, cellular landscape  +, landscape evolution  +, emphasis on fluvial  +, grainsize sediment  +  and caesar  +
As code  +  and As teaching tool  +
landscape evolution  +
Modular  +
http://www.coulthard.org.uk  +
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02:16:03, 17 September 2020  +
69  +
Cellular landscape evolution model  +
Cottingham Road  +
HU6 7RX  +
5 min to 50 days  +
Through web repository  +
http://www.coulthard.org.uk/downloads/visualcaesar.htm  +
NO STATE  +
Linux  +  and Windows  +
Model developer  +