Topographic Wetness Index (One Step)
- Author: O.Conrad (c) 2014
 
- Menu: Terrain Analysis | Hydrology | Topographic Indices
 
Description
		Calculates the Topographic Wetness Index (TWI) based on the supplied Digital Elevation Model (DEM). Slopes (Beta), Specific Catchment Areas (SCA), and a depressionless DEM for SCA calculation are derived internally.
		TWI = ln(SCA / tan(Beta))
	
References
- Beven, K.J., Kirkby, M.J. (1979): A physically-based variable contributing area model of basin hydrology. Hydrology Science Bulletin 24(1), p.43-69.
 - Moore, I.D., Grayson, R.B., Ladson, A.R. (1991): Digital terrain modelling: a review of hydrogical, geomorphological, and biological applications. Hydrological Processes, Vol.5, No.1.
 
Parameters
|   | Name | Type | Identifier | Description | Constraints | 
| Input | Elevation | grid, input | DEM | - | - | 
| Output | Topographic Wetness Index | grid, output | TWI | - | - | 
| Options | Grid System | grid system | GRID_SYSTEM | - | - | 
| Preprocessing | choice | PREPROCESSING | - | Available Choices:
[0] Fill Sinks (Wang & Liu)
[1] Sink Removal
Default: 0 | 
| Flow Routing | choice | FLOW_METHOD | - | Available Choices:
[0] Deterministic 8
[1] Rho 8
[2] Braunschweiger Reliefmodell
[3] Deterministic Infinity
[4] Multiple Flow Direction
[5] Multiple Triangular Flow Direction
[6] Multiple Maximum Downslope Gradient Based Flow Direction
Default: 0 | 
Command Line
Usage: saga_cmd ta_hydrology twi [-DEM ] [-TWI ] [-PREPROCESSING ] [-FLOW_METHOD ]
  -DEM:             Elevation
	grid, input
  -TWI:             Topographic Wetness Index
	grid, output
  -PREPROCESSING:
                         Preprocessing
                         	choice
                         	Available Choices:
                         	[0] Fill Sinks (Wang & Liu)
                         	[1] Sink Removal
                         	Default: 0
  -FLOW_METHOD:
                         Flow Routing
                         	choice
                         	Available Choices:
                         	[0] Deterministic 8
                         	[1] Rho 8
                         	[2] Braunschweiger Reliefmodell
                         	[3] Deterministic Infinity
                         	[4] Multiple Flow Direction
                         	[5] Multiple Triangular Flow Direction
                         	[6] Multiple Maximum Downslope Gradient Based Flow Direction
                         	Default: 0