This tool estimates the flow distribution at a specified time after a rainfall event. It is based on a standard flow accumulation calculation (e.g. O'Callaghan & Mark 1984, Freeman 1991) that has an additional function to accumulate the flow travel time. Final flow accumulation becomes that part of the total flow through that corresponds to the portion of flow travel time that exceeds the targeted time. The travel time is estimated with the empirical Manning equation (e.g. Dingman 1994, Freeman et al. 1998, Manning 1891).
| Name | Type | Identifier | Description | Constraints |
Input | Elevation | Grid (input) | DEM | [m] | - |
Manning-Strickler Coefficient (*) | Grid (optional input) | FLOW_K | Manning-Strickler coefficient for flow travel time estimation (reciprocal of Manning's Roughness Coefficient) | - |
Output | Flow Accumulation | Grid (output) | FLOW_ACC | [mm] | - |
Flow Through (*) | Grid (optional output) | FLOW | - | - |
Flow Travel Time (*) | Grid (optional output) | TIME_MEAN | - | - |
Flow Concentration (*) | Grid (optional output) | TIME_CONC | - | - |
Flow Velocity (*) | Grid (optional output) | VELOCITY | - | - |
Options | Grid System | Grid system | PARAMETERS_GRID_SYSTEM | - | - |
Default | Floating point | FLOW_K_DEFAULT | default value if no grid has been selected | Minimum: 0.000000 Default: 20.000000 |
Time | Floating point | TIME | minutes | Minimum: 0.001000 Default: 5.000000 |
Flow Routing | Choice | ROUTING | - | Available Choices: [0] D8 [1] MFD Default: 1 |
Flow Depth | Choice | FLOW_DEPTH | - | Available Choices: [0] constant [1] dynamic Default: 1 |
Constant Flow Depth | Floating point | FLOW_CONST | [mm] | Minimum: 0.000000 Default: 10.000000 |
Reset | Boolean | RESET | Resets flow accumulation raster. | Default: 1 |
Rain | Floating point | RAIN | The flow portion [mm] added to each raster cell before simulation starts. | Minimum: 0.000000 Default: 10.000000 |
(*) optional |