The parameters of a simulation are given through a configuration file in a format similar to Microsoft Windows INI files. An example is given in the tutorial above. The file is separated in sections described below.
Simulation duration could be given by a combination of start time, end time and duration. If only the duration is given, the results will be written as a relative time STRDS. In case start time is given, the simulation will use an absolute temporal type.
|start_time||Starting time||yyyy-mm-dd HH:MM|
|end_time||Ending time||yyyy-mm-dd HH:MM|
|record_step||Time-step at which results are written to the disk||HH:MM:SS|
- start_time and end_time
- start_time and duration
- duration only
Itzï does not support Lat-Long coordinates. A projected location should be used. The inputs maps could be given either as STRDS or single maps. First, the module try to load a STRDS of the given name. If unsuccessful, it will load the given map, and stop with an error if the name does not correspond to either a map or a STRDS.
The following inputs are mandatory:
- Digital elevation model in meters
- Friction, expressed as Manning’s n
|dem||Elevation in meters||map or strds|
|friction||Manning’s n (friction coefficient)||map or strds|
|start_h||Starting water depth in meters||map name|
|rain||Rainfall in mm/h||map or strds|
|inflow||Point inflow in m/s (ex: for 20 m3/s on a 10x10 cell, velocity is 0.2 m/s)||map or strds|
|bctype||Boundary conditions type||map or strds|
|bcval||Boundary conditions values||map or strds|
|infiltration||Fixed infiltration rate in mm/h||map or strds|
|effective_pororosity||Effective porosity in mm/mm||map or strds|
|capillary_pressure||Wetting front capillary pressure head in mm||map or strds|
|hydraulic_conductivity||Soil hydraulic conductivity in mm/h||map or strds|
|drainage_capacity||Drainage capacity in mm/h (new in 16.9)||map or strds|
Boundary conditions type are defined by an integer as follow:
- 0 or 1: Closed boundary (default)
- 2: Open boundary: velocity at the boundary is equal to the velocity inside the domain
- 3: Not implemented yet
- 4: User-defined water depth inside the domain
The “open” and “closed” boundary conditions are applied only at the border of the GRASS computational region.
infiltration and any of the Green-Ampt parameters are mutually exclusives. Likewise, if any of the Green-Ampt parameter is given, all the others should be given as well.
|prefix||Prefix of output STRDS||string|
|values||Values to be saved. Each one will be a STRDS||comma separated list|
The possible values to be exported are the following:
|wse||Water surface elevation (depth + elevation)||meters|
|v||Overland flow speed (velocity’s magnitude)||m/s|
|vdir||Velocity’s direction. CCW from East||degrees|
|qx||Volumetric flow, x direction. Positive if going East||m³/s|
|qy||Volumetric flow, y direction. Positive if going South||m³/s|
|boundaries||Flow coming in (positive) or going out (negative) the domain due to boundary conditions. Average since the last record||m/s|
|infiltration||Infiltration rate. Average since the last record||mm/h|
|rainfall||Rainfall rate. Average since the last record||mm/h|
|inflow||Average user flow since the last record||m/s|
|drainage_cap||Average flow due to drainage capacity since the last record (new in 17.1)||m/s|
|verror||Total created volume due to numerical error since the last record (new in 17.1)||m³|
New in version 17.1: drainage_cap and verror are added.
Additionally to output a map at each record_step, h and v also produce a map of maximum values.
Water depth maps, apart from map of maximum values, do not display values under the hmin threshold (See below). When the exported map is totally empty, it is deleted at the end of the simulation.
|stats_file||Statistics file||CSV table|
Changed in version 17.1: Mass balance calculation now takes into account the volume from drainage capacity. Created volume calculation is changed.
The statistic file is presented as a CSV file and updated at each record_step. The values exported are shown in the table below.
Water entering the domain is represented by a positive value. Water that leaves the domain is negative. Volumes are in m³.
|sim_time||Elapsed simulation time|
|avg_timestep||Average time-step duration since last record|
|#timesteps||Number of time-steps since the last record|
|boundary_vol||Water volume that passed the domain boundaries since last record|
|rain_vol||Rain volume that entered the domain since last record|
|inf_vol||Water volume that left the domain due to infiltration since last record|
|inflow_vol||Water volume that entered or left the domain due to user inflow since last record|
|drain_cap_vol vol||Water volume that entered or left the domain due to drainage capacity since last record|
|domain_vol||Total water volume in the domain at this time-step|
|created_vol||Water volume created due to numerical errors since last record record|
|%error||Percentage of the domain volume variation due to numerical error. Corresponds to created_vol / (domain_vol - old_domain_vol) * 100|
|hmin||Water depth threshold in metres||positive float||0.005|
|cfl||Coefficient applied to calculate time-step||positive float||0.7|
|theta||Inertia weighting coefficient||float between 0 and 1||0.9|
|vrouting||Routing velocity in m/s||positive float||0.1|
|dtmax||Maximum surface flow time-step in seconds||positive float||5|
|dtinf||Time-step of infiltration, drainage capacity and rainfall. In seconds||positive float||60|
When water depth is under hmin, the flow is routed at the fixed velocity defined by vrouting.
New in version 16.9.
Setting those parameters allows to run simulation outside the GRASS shell. This is especially useful for batch processing involving different locations and mapsets. If Itzï is run from within the GRASS shell, this section is not necessary.
|grass_bin||Path to the grass binary||string|
|grassdata||Full path to the GIS DataBase||string|
|location||Name of the location||string|
|mapset||Name of the mapset||string|
With Linux, grass_bin could be simply “grass”.