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:
Input DEM raster dataset
Output raster name and format
Outputs:
A Floating raster representing the Flow Direction according to the
D-infinity (Deterministic Infinity) method.
Example:
An example of Flow Direction D-infinity output.
Notes:
The D-infinity method was suggested by Tarboton (1997). In it Flow Direction is defined
as the angle of the steepest descent determined by analysis of 8 triangular facets formed by
the 3x3 cell neighborhood.
The flow direction values are in Decimal Degrees from 0 to 360.0.
The value of 0.0 indicates an outlet and all other values represent the
direction of flow starting from North in clockwise direction.
For example a value of 90 indicates flow to the East and a value of 225 - flow to South West.
The D-infinity method allows flow divergence - the flow
from a cell will either go to one or two of the neighboring cells.This is a better representation of water flow on divergent slopes.
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