[GRASSLIST:5644] Re: r.flow and flowpath length
Jaro Hofierka
hofierka at geomodel.sk
Sun Feb 23 00:19:43 EST 2003
Marco,
r.fill.dir is based on D8 algorithm, while r.flow is based on D-infinity
algorithm. Therefore r.fill.dir cannot create a fully depression-free
DEM for r.flow. This explains at least part of your problems.
A short example of how to fix the problem and create hydrologically
correct DEMs can be found in this paper available online:
Cebecauer, T., Hofierka, J., Šúri, M. (2002). Processing digital terrain
models by regularized spline with tension: tuning interpolation
parameters for different input datasets. Proceeding of conference "Open
source GIS - GRASS users conference 2002", Trento (Italy), 11.-13. 9. 2002.
http://www.ing.unitn.it/~grass/conferences/GRASS2002/proceedings/pdfs/Cebecauer_Tomas.pdf
Kind regards,
Jaro
marco castrogiovanni wrote:
> hi,
> I'm currently building up an hydrologic model based on raindrop method.
> I need to calculate the lengths of flowlines. I've tried with r.flow by
> the following syntax:
>
> r.flow -3 elevin=bas.dem aspin=bas.asp flout= bas.flow lgout=bas.len
>
> where bas.dem is a raster map (filled with r.fill.dir) with resolution
> of 1920x2100 cells, with cell-dimensions 20x20 meters and with high
> precision quota value (six decimal numbers).
> I haven't obtained any acceptable results yet, 'cause all flowlines
> suddenly stop in unexpected points and they don't reach the outlet.
> Raster map of distances from outlet that I get after running r.flow
> have a lot of zero-value cells, but their corresponding quota and
> aspect value wouldn't allow these results.
> Any suggestions would be appreciated.
>
> Regards, Marco.
>
>
>
>
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