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r.fill.dir(1grass)          GRASS GIS User's Manual         r.fill.dir(1grass)

NAME
       r.fill.dir   - Filters and generates a depressionless elevation map and
       a flow direction map from a given elevation raster map.

KEYWORDS
       raster, hydrology, sink, fill sinks, depressions

SYNOPSIS
       r.fill.dir
       r.fill.dir --help
       r.fill.dir [-f]  input=name  output=name  direction=name   [areas=name]
       [format=string]     [--overwrite]    [--help]   [--verbose]   [--quiet]
       [--ui]

   Flags:
       -f
           Find unresolved areas only

       --overwrite
           Allow output files to overwrite existing files

       --help
           Print usage summary

       --verbose
           Verbose module output

       --quiet
           Quiet module output

       --ui
           Force launching GUI dialog

   Parameters:
       input=name [required]
           Name of input elevation raster map

       output=name [required]
           Name for output depressionless elevation raster map

       direction=name [required]
           Name for output flow direction  map  for  depressionless  elevation
           raster map

       areas=name
           Name for output raster map of problem areas

       format=string
           Aspect direction format
           Options: agnps, answers, grass
           Default: grass

DESCRIPTION
       r.fill.dir  filters  and generates a depressionless elevation map and a
       flow direction map from a  given  raster  elevation  map.   The  method
       adopted  to filter the elevation map and rectify it is based on the pa-
       per titled "Extracting topographic  structure  from  digital  elevation
       model  data  for geographic information system analysis" by S.K. Jenson
       and J.O. Domingue (1988).

       The procedure takes an elevation layer as input and initially fills all
       the  depressions  with one pass across the layer. Next, the flow direc-
       tion algorithm tries to find a unique direction for each cell.  If  the
       watershed program detects areas with pothholes, it delineates this area
       from the rest of the area and once again the depressions are filled us-
       ing  the neighborhood technique used by the flow direction routine. The
       final output will be a depressionless elevation layer and a unique flow
       direction layer.

       This  (D8)  flow algorithm performs as follows: At each raster cell the
       code determines the slope to each of the 8 surrounding  cells  and  as-
       signs  the  flow  direction  to  the highest slope out of the cell.  If
       there is more than one equal, non-zero slope then the  code  picks  one
       direction  based  on  preferences that are hard-coded into the program.
       If the highest slope is flat and in more than one  direction  then  the
       code  first  tries to select an alternative based on flow directions in
       the adjacent cells. r.fill.dir iterates that process, effectively prop-
       agating  flow directions from areas where the directions are known into
       the area where the flow direction cannot otherwise be resolved.

       The format parameter is the type of format at which the user wishes  to
       create  the  flow direction map.  The flow direction map can be encoded
       in GRASS GIS aspect format, ANSWERS (Beasley  et.al,  1982),  or  AGNPS
       (Young  et.al, 1985) format, so that it can be readily used as input to
       other GRASS GIS modules or the aforementioned hydrological models.  The
       grass format gives the same category values as r.slope.aspect gives for
       aspect, i.e. angles in degrees counter-clockwise from east in 45 degree
       increments.   The  agnps  format gives category values from 1-8, with 1
       facing north and increasing values in the clockwise direction.  The an-
       swers  format  gives category values from 0-360 degrees, with 0 (repre-
       sented as 360) facing east and values increasing in the  counter-clock-
       wise  direction  at 45 degree increments.  In all cases, NULL (no data)
       values are used for cells where direction cannot be determined.

       In case of local problems, those unfilled areas can be  stored  option-
       ally.   Each  unfilled  area  in this maps is numbered. The -f flag in-
       structs the program to fill single-cell pits but otherwise to just find
       the  undrained  areas and exit. With the -f flag set the program writes
       an elevation map with just single-cell pits  filled,  a  direction  map
       with  unresolved  problems  and  a map of the undrained areas that were
       found but not filled. This option was included because filling DEMs was
       often  not  the best way to solve a drainage problem. These options let
       the user get a partially-fixed elevation map,  identify  the  remaining
       problems and fix the problems appropriately.

       In  some  cases it may be necessary to run r.fill.dir repeatedly (using
       output from one run as input to the next run) before all of problem ar-
       eas are filled.

       The  resulting  depressionless elevation raster map can further be pro-
       cessed to derive slopes and other attributes required by  other  hydro-
       logical models.

       As  any  GRASS GIS module, r.fill.dir is sensitive to the computational
       region settings. Thus the module can be used to generate a flow  direc-
       tion  map  for any sub-area within the full map layer. Also, r.fill.dir
       is sensitive to any raster MASK in effect.

NOTES
           •   The r.fill.dir module can be used not only to fill  depression,
               but also to detect water bodies or potential water bodies based
               on the nature of the terrain and the  digital  elevation  model
               used.

           •   Not  all depressions are errors in digital elevation models. In
               fact, many are wetlands and as Jenkins and McCauley (2006) note
               careless  use of depression filling may lead to unintended con-
               sequences such as loss of wetlands.

           •   Although many hydrological algorithms require depression  fill-
               ing,  advanced algorithms such as those implemented in r.water-
               shed and r.sim.water do not require depressionless digital ele-
               vation model to work.

           •   The flow direction map can be visualized with d.rast.arrow.

EXAMPLES
       Generic  example:  create  a  depressionless  (sinkless)  elevation map
       ansi.fill.elev and a flow direction map ansi.asp for the type "grass":
       r.fill.dir input=ansi.elev output=ansi.fill.elev direction=ansi.asp

       North Carolina sample dataset example: The LiDAR derived  1m  elevation
       map is sink-filled. The outcome are a depressionless elevation map, the
       flow direction map and an error map.
       # set computational region to elevation map
       g.region raster=elev_lid792_1m -p
       # generate depressionless DEM and related maps
       r.fill.dir input=elev_lid792_1m output=elev_lid792_1m_filled \
                  direction=elev_lid792_1m_dir areas=elev_lid792_1m_error
       # generate elevation map of pixelwise differences to see obtained terrain alterations
       r.mapcalc "elev_lid792_1m_diff = elev_lid792_1m_filled - elev_lid792_1m"
       r.colors elev_lid792_1m_diff color=differences
       # assess univariate statistics of differences
       r.univar -e elev_lid792_1m_diff
       # vectorize filled areas (here all fills are of positive value, see r.univar output)
       r.mapcalc "elev_lid792_1m_fill_area = if(elev_lid792_1m_diff > 0.0, 1, null() )"
       r.to.vect input=elev_lid792_1m_fill_area output=elev_lid792_1m_fill_area type=area
       # generate shaded terrain for better visibility of results
       r.relief input=elev_lid792_1m_filled output=elev_lid792_1m_filled_shade
       d.mon wx0
       d.shade shade=elev_lid792_1m_filled_shade color=elev_lid792_1m_filled
       d.vect elev_lid792_1m_fill_area type=boundary color=red
       Figure: Sink-filled DEM (shown as shaded terrain) with areas of filling
       shown as vector polygons

REFERENCES
           •   Beasley,  D.B.  and L.F. Huggins. 1982. ANSWERS (areal nonpoint
               source watershed  environmental  response  simulation):  User’s
               manual. U.S. EPA-905/9-82-001, Chicago, IL, 54 p.

           •   Jenkins,  D.  G.,  and McCauley, L. A. 2006.  GIS, SINKS, FILL,
               and disappearing wetlands: unintended consequences in algorithm
               development  and use.  In Proceedings of the 2006 ACM symposium
               on applied computing (pp. 277-282).

           •   Jenson, S.K., and J.O. Domingue. 1988.  Extracting  topographic
               structure  from digital elevation model data for geographic in-
               formation system analysis. Photogram.  Engr. and  Remote  Sens.
               54: 1593-1600.

           •   Young,  R.A.,  C.A. Onstad, D.D. Bosch and W.P. Anderson. 1985.
               Agricultural nonpoint surface pollution models (AGNPS) I and II
               model  documentation.  St. Paul: Minn. Pollution control Agency
               and Washington D.C., USDA-Agricultural Research Service.

SEE ALSO
        d.rast.arrow, d.shade, g.region, r.fillnulls, r.relief, r.slope.aspect

AUTHORS
       Fortran version: Raghavan Srinivasan, Agricultural Engineering  Depart-
       ment, Purdue University
       Rewrite to C with enhancements: Roger S. Miller

SOURCE CODE
       Available at: r.fill.dir source code (history)

       Accessed: unknown

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       © 2003-2022 GRASS Development Team, GRASS GIS 7.8.7 Reference Manual

GRASS 7.8.7                                                 r.fill.dir(1grass)

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