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NAME - Create a raster map from an assemblage of many coordinates using univariate statistics.



SYNOPSIS help [-sg] input=name output=name [method=string] [type=string] [fs=character] [x=integer] [y=integer] [z=integer] [zrange=min,max] [percent=integer] [--overwrite]


Scan data file for extent then exit
In scan mode, print using shell script style
Force overwrite of output files


ASCII file containing input data
Name for output raster map
Statistic to use for raster values
Options: n,min,max,range,sum,mean,stddev,variance,coeff_var
Default: mean
Storage type for resultant raster map
Default: FCELL
Field separator
Default: |
Column number of x coordinates in input file (first column is 1)
Default: 1
Column number of y coordinates in input file
Default: 2
Column number of data values in input file
Default: 3
Filter range for z data (min,max)
Percent of map to keep in memory
Options: 1-100
Default: 100


The module will load and bin ungridded x,y,z ASCII data into a new raster map. The user may choose from a variety of statistical methods in creating the new raster. is designed for processing massive point cloud datasets, for example raw LIDAR or sidescan sonar swath data.

Available statistics for populating the raster are:


Memory use

While the input file can be arbitrarily large, will use a large amount of system memory for large raster regions (10000x10000). If the module refuses to start complaining that there isn't enough memory, use the percent parameter to run the module in several passes. In addition using a less precise map format (CELL [integer] or FCELL [floating point]) will use less memory than a DCELL [double precision floating point] output map. Methods such as n, min, max, sum will also use less memory, while stddev, variance, and coeff_var will use more. The default map type=FCELL is intended as compromise between preserving data precision and limiting system resource consumption.

Setting region bounds and resolution

You can use the -s scan flag to find the extent of the input data (and thus point density) before performing the full import. Use g.region to adjust the region bounds to match. The -g shell style flag prints the extent suitable as parameters for g.region. A suitable resolution can be found by dividing the number of input points by the area covered. e.g.
  wc -l inputfile.txt
  g.region -p
  # points_per_cell = n_points / (rows * cols)

  g.region -e
  # UTM location:
  # points_per_sq_m = n_points / (ns_extent * ew_extent)

  # Lat/Lon location:
  # points_per_sq_m = n_points / (ns_extent * ew_extent*cos(lat) * (1852*60)^2)

If you only intend to interpolate the data with and, then there is little point to setting the region resolution so fine that you only catch one data point per cell -- you might as well use " -zbt" directly.


Points falling outside the current region will be skipped. This includes points falling exactly on the southern region bound. (to capture those adjust the region with "g.region s=s-0.000001"; see g.region)

Blank lines and comment lines starting with the hash symbol (#) will be skipped.

The zrange parameter may be used for filtering the input data by vertical extent. Example uses might include preparing multiple raster sections to be combined into a 3D raster array with, or for filtering outliers on relatively flat terrain.

In varied terrain the user may find that min maps make for a good noise filter as most LIDAR noise is from premature hits. The min map may also be useful to find the underlying topography in a forested or urban environment if the cells are over sampled.

The user can use a combination of output maps to create custom filters. e.g. use r.mapcalc to create a mean-(2*stddev) map. [In this example the user may want to include a lower bound filter in r.mapcalc to remove highly variable points (small n) or run r.neighbors to smooth the stddev map before further use.]


If the raster map is to be reprojected, it may be more appropriate to reproject the input points with m.proj or cs2cs before running

Interpolation into a DEM

The vector engine's topographic abilities introduce a finite memory overhead per vector point which will typically limit a vector map to approximately 3 million points (~ 1750^2 cells). If you want more, use the -b flag to skip building topology. Without topology, however, all you'll be able to do with the vector map is display with d.vect and interpolate with Run r.univar on your raster map to check the number of non-NULL cells and adjust bounds and/or resolution as needed before proceeding.

Typical commands to create a DEM using a regularized spline fit:

  r.univar lidar_min -z feature=point in=lidar_min out=lidar_min_pt layer=0 in=lidar_min_pt elev=lidar_min.rst


Import the Jockey's Ridge, NC, LIDAR dataset, and process into a clean DEM:
    # scan and set region bounds -s fs=, in=lidaratm2.txt out=test
  g.region n=35.969493 s=35.949693 e=-75.620999 w=-75.639999
  g.region res=0:00:00.075 -a
    # create "n" map containing count of points per cell for checking density in=lidaratm2.txt out=lidar_n fs=, method=n zrange=-2,50
    # check point density [rho = n_sum / (rows*cols)]
  r.univar lidar_n | grep sum
    # create "min" map (elevation filtered for premature hits) in=lidaratm2.txt out=lidar_min fs=, method=min zrange=-2,50
    # zoom to area of interest
  g.region n=35:57:56.25N s=35:57:13.575N w=75:38:23.7W e=75:37:15.675W
    # check number of non-null cells (try and keep under a few million)
  r.univar lidar_min | grep '^n:'
    # convert to points -z feature=point in=lidar_min out=lidar_min_pt
    # interpolate using a regularized spline fit layer=0 in=lidar_min_pt elev=lidar_min.rst
    # set color scale to something interesting
  r.colors lidar_min.rst rule=bcyr
    # prepare a 1:1:1 scaled version for NVIZ visualization (for lat/lon input)
  r.mapcalc "lidar_min.rst_scaled = lidar_min.rst / (1852*60)"
  r.colors lidar_min.rst_scaled rule=bcyr



If you encounter any problems (or solutions!) please contact the GRASS Development Team.


g.region, m.proj, r.fillnulls,, r.mapcalc, r.neighbors,,, r.univar, r.univar2,,


Hamish Bowman
Department of Marine Science
University of Otago
New Zealand

Last changed: $Date: 2006/06/17 06:23:49 $

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