Flow Direction D-infinity

Running programmatically

Generates a Flow Direction raster in which each cells represents the direction of flow for this cell in the DEM using the D-infinity method.

Inputs:

Outputs:

Example:

An example of Flow Direction D-infinity output.

Notes:

Running Programmatically

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Parameters

Expression Explanation
Function Name FlowDirectionDinf
<input raster> A String representing the input DEM raster dataset.
<output raster> A String - the full name of the output raster.

Running the function

ETSPath used in the table below is the full path to ETSRun.exe (E.G. "C:\Program Files\ETSpatial Techniques\ETSurface\ETSRun.exe")

UnitsDegrees
Language Syntax
Python subprocess.call([ETSPath, "FlowDirectionDinf", "input raster", "output raster"])
.NET using ETSRun.exe StartInfo.FileName = ETSPath
StartInfo.Arguments = "FlowDirectionDinf" "input raster" "output raster"
.NET using ETSOutX.dll FlowDirectionDinf(input raster, output raster)
ArcPy arcpy.FlowDirectionDinf("input raster", "output raster")

Notes:

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Reference:

Tarboton, D. G., (1997),"A New Method for the Determination of Flow Directions and Contributing Areas in Grid Digital Elevation Models", Water Resources Research, 33(2): 309-319