On
17/04/2019 19:34, Mehrdad Varedi wrote:
Hi Everyone,
I would like to know how the flow path, flow
accumulation, or topographic wetness is calculated in
cities versus farms.
In other words how to take into account the effect
of non-penetrable areas in forming the above-mentioned
layers based on a DEM and penetrability score for the
study area?
No answers yet, so I will give a try:
Each of the variables in your question are geomorphology
characteristics. They depend only on elevation, slope,
aspect. Flow accumulation is an area, TWI is area divided
by tan(slope), etc. These characteristics have nothing to
do with infiltration (i.e. penetrable areas).
Having said that, the GRASS module r.watershed can take
two input rasters: flow and retention, which change the
output flow accumulation. If you have spatial data on soil
retention properties, or disturbances to surface flow, you
can apply them to r.watershed to get a more "realistic"
accumulation grid. The defaults are 100 for retention (no
infiltration, all water flowing into a cell also goes out)
and 1.0 for flow (no disturbances, and no additional
contribution for each cell)
Thanks for your help,
Mehrdad
ᐧ
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Micha Silver
Ben Gurion Univ.
Sde Boker, Remote Sensing Lab
+972-523-665918