SAGA 9.14.0 | Tool Documentation

Upslope Area

Author(s) O.Conrad (c) 2001
Library IDta_hydrology
Tool ID 3
Version 1.0
Menu Terrain Analysis | Hydrology | Flow Accumulation

Description

This tool allows you to specify target cells, for which the upslope contributing area shall be identified. The result will give for each cell the percentage of its flow that reaches the target cell(s). _______ Interactive version (left mouse clicks will trigger the calculation for the selected cell).

References

Freeman, G.T. (1991): Calculating catchment area with divergent flow based on a regular grid. Computers and Geosciences, 17:413-22.

O'Callaghan, J.F. & Mark, D.M. (1984): The extraction of drainage networks from digital elevation data. Computer Vision, Graphics and Image Processing, 28:323-344.

Qin, C. Z., Zhu, A. X., Pei, T., Li, B. L., Scholten, T., Behrens, T. & Zhou, C. H. (2011): An approach to computing topographic wetness index based on maximum downslope gradient. Precision Agriculture, 12(1), 32-43. ResearchGate

Quinn, P.F., Beven, K.J., Chevallier, P. & Planchon, O. (1991): The prediction of hillslope flow paths for distributed hydrological modelling using digital terrain models. Hydrological Processes, 5:59-79. ResearchGate

Seibert, J. & McGlynn, B. (2007): A new triangular multiple flow direction algorithm for computing upslope areas from gridded digital elevation models. Water Resources Research, Vol. 43, W04501,
C++ implementation in SAGA by Thomas Grabs (c) 2007, contact: thomas.grabs@natgeo.su.se, jan.seibert@natgeo.su.se. Wiley

Tarboton, D.G. (1997): A new method for the determination of flow directions and upslope areas in grid digital elevation models. Water Resources Research, Vol.33, No.2, p.309-319. Wiley

Parameters

 NameTypeIdentifierDescriptionConstraints
InputElevationgrid, inputELEVATION--
Sink Routesgrid, input, optionalSINKROUTE--
OutputUpslope Areagrid, outputAREA--
OptionsMethodchoiceMETHOD-Available Choices: [0] Deterministic 8 [1] Deterministic Infinity [2] Multiple Flow Direction [3] Multiple Triangular Flow Direction [4] Multiple Maximum Downslope Gradient Based Flow Direction Default: 2
Convergencefloating point numberCONVERGEConvergence factor for Multiple Flow Direction algorithmMinimum: 0.001000 Default: 1.1
Contour LengthbooleanMFD_CONTOURInclude (pseudo) contour length as additional weighting factor in multiple flow direction routing, reduces flow to diagonal neighbour cells by a factor of 0.71 (s. Quinn et al. 1991 for details).Default: 0

Command Line

This tool is not intended to be run from the command line!