SAGA 9.12.4 | Tool Documentation

Topographic Wetness Index (One Step)

Author(s) O.Conrad (c) 2014
Library IDta_hydrology
Tool ID twi
Version 1.0
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

 NameTypeIdentifierDescriptionConstraints
InputElevationgrid, inputDEM--
OutputTopographic Wetness Indexgrid, outputTWI--
OptionsGrid Systemgrid systemGRID_SYSTEM--
PreprocessingchoicePREPROCESSING-Available Choices: [0] Fill Sinks (Wang & Liu) [1] Sink Removal Default: 0
Flow RoutingchoiceFLOW_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