grdhisteq man page on DragonFly

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GRDHISTEQ(1)		     Generic Mapping Tools		  GRDHISTEQ(1)

NAME
       grdhisteq - Histogram equalization for grid files

SYNOPSIS
       grdhisteq  in_grdfile [ -Gout_grdfile ] [ -Cn_cells ] [ -D ] [ -N[norm]
       ] [ -Q ] [ -V ]

DESCRIPTION
       grdhisteq allows the user to find the data values which divide a	 given
       grid  file  into patches of equal area.	One common use of grdhisteq is
       in a kind of histogram equalization of an image.	 In this  application,
       the  user  might	 have a grid of flat topography with a mountain in the
       middle.	Ordinary gray shading of this  file  (using  grdimage/grdview)
       with  a	linear mapping from topography to graytone will result in most
       of the image being very dark  gray,  with  the  mountain	 being	almost
       white.	One  could  use	 grdhisteq to write to stdout an ASCII list of
       those data values which divide the range of the data into n_cells  seg‐
       ments,  each  of	 which	has  an equal area in the image.  Using awk or
       makecpt one can take this output and build a cpt file; using  the  cpt‐
       file  with  grdimage  will  result  in an image with all levels of gray
       occurring equally.  Alternatively, see grd2cpt.

       The second common use of grdhisteq is in writing a grid with statistics
       based on some kind of cumulative distribution function.	In this appli‐
       cation, the output has relative highs and lows in the same (x,y)	 loca‐
       tions  as  the  input file, but the values are changed to reflect their
       place in some cumulative distribution.  One example would  be  to  find
       the lowest 10% of the data:  Take a grid, run grdhisteq and make a grid
       using n_cells = 10, and then contour the result to trace the 1 contour.
       This will enclose the lowest 10% of the data, regardless of their orig‐
       inal values.  Another example is in equalizing the output of  grdgradi‐
       ent.   For  shading  purposes it is desired that the data have a smooth
       distribution, such as a gaussian.  If you run grdhisteq on output  from
       grdgradient  and	 make a grid file output with the Gaussian option, you
       will have a grid whose values are distributed according to  a  gaussian
       distribution  with zero mean and unit variance.	The locations of these
       values will correspond to the locations of the input; that is, the most
       negative	 output	 value will be in the (x,y) location of the most nega‐
       tive input value, and so on.

       in_grdfile
	      2-D binary grid file to be equalized.  (See  GRID	 FILE  FORMATS
	      below).

OPTIONS
       No space between the option flag and the associated arguments.

       -C     Sets how many cells (or divisions) of data range to make.

       -D     Dump level information to standard output.

       -G     Name  of	output	2-D  grid file.	 Used with -N only.  (See GRID
	      FILE FORMATS below).

       -N     Gaussian output.	Use with -G to make an output grid with	 stan‐
	      dard  normal scores.  Append norm to force the scores to fall in
	      the <-1,+1> range [Default is standard normal scores].

       -Q     Use quadratic intensity scaling.	[Default is linear].

       -V     Selects verbose mode, which will send progress reports to stderr
	      [Default runs "silently"].

GRID FILE FORMATS
       By  default GMT writes out grid as single precision floats in a COARDS-
       complaint netCDF file format.  However, GMT is  able  to	 produce  grid
       files  in  many	other commonly used grid file formats and also facili‐
       tates so called "packing" of grids, writing out floating point data  as
       2-  or 4-byte integers. To specify the precision, scale and offset, the
       user should add the suffix =id[/scale/offset[/nan]], where id is a two-
       letter  identifier of the grid type and precision, and scale and offset
       are optional scale factor and offset to be applied to all grid  values,
       and  nan	 is  the  value	 used  to indicate missing data.  When reading
       grids, the format is generally automatically recognized.	 If  not,  the
       same  suffix can be added to input grid file names.  See grdreformat(1)
       and Section 4.17 of the GMT Technical Reference and Cookbook  for  more
       information.

       When reading a netCDF file that contains multiple grids, GMT will read,
       by default, the first 2-dimensional grid that can find in that file. To
       coax  GMT  into	reading another multi-dimensional variable in the grid
       file, append ?varname to the file name, where varname is	 the  name  of
       the variable. Note that you may need to escape the special meaning of ?
       in your shell program by putting a backslash in	front  of  it,	or  by
       placing	the  filename and suffix between quotes or double quotes.  The
       ?varname suffix can also be used for output grids to specify a variable
       name  different	from the default: "z".	See grdreformat(1) and Section
       4.18 of the GMT Technical Reference and Cookbook for more  information,
       particularly on how to read splices of 3-, 4-, or 5-dimensional grids.

EXAMPLES
       To  find	 the height intervals that divide the file heights.grd into 16
       divisions of equal area:

       grdhisteq heights.grd -C 16 -D > levels.d

       To make the poorly distributed intensities in the  file	raw_intens.grd
       suitable for use with grdimage or grdview, run

       grdhisteq raw_intens.grd -G smooth_intens.grd -N -V

RESTRICTIONS
       If  you use grdhisteq to make a gaussian output for gradient shading in
       grdimage or grdview, you should be aware of the following:  the	output
       will be in the range [-x, x], where x is based on the number of data in
       the input grid (nx * ny) and the cumulative gaussian distribution func‐
       tion  F(x).  That is, let N = nx * ny.  Then x will be adjusted so that
       F(x) = (N - 1 + 0.5)/N.	Since about 68% of the values from a  standard
       normal  distribution fall within +/- 1, this will be true of the output
       grid.  But if N is very large, it is possible for x to be greater  than
       4.   Therefore,	with  the  grdimage  program clipping gradients to the
       range [-1, 1], you will get correct shading of 68% of your data,	 while
       16%  of	them  will be clipped to -1 and 16% of them clipped to +1.  If
       this makes too much of the image too light or too dark, you should take
       the output of grdhisteq and rescale it using grdmath and multiplying by
       something less than 1.0, to shrink the range of the values, thus bring‐
       ing  more than 68% of the image into the range [-1, 1].	Alternatively,
       supply a normalization factor with -N.

SEE ALSO
       gmtdefaults(1), GMT(1), grd2cpt(1), grdgradient(1),  grdimage(1),  grd‐
       math(1), grdview(1), makecpt(1)

GMT 4.5.14			  1 Nov 2015			  GRDHISTEQ(1)
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