Provided by: gmt-common_5.2.1+dfsg-3build1_all bug

NAME

       hotspotter - Create CVA image from seamount locations

SYNOPSIS

       hotspotter  [tables] rotfile CVAgrid increment region [ upper_age ] [  ] [  ] [ [level] ] [ -bi<binary> ]
       [ -di<nodata> ] [ -h<headers> ] [ -i<flags> ] [ -o<flags> ] [ -:[i|o] ]

       Note: No space is allowed between the option flag and the associated arguments.

DESCRIPTION

       hotspotter reads (longitude, latitude, amplitude, radius, age) records from tables  [or  standard  input]
       and calculates flowlines using the specified stage or total reconstruction rotations. These flowlines are
       convolved  with  the  shape of the seamount (using a Gaussian shape given amplitude and radius = 6 sigma)
       and added up to give  a  Cumulative  Volcano  Amplitude  grid  (CVA).  See  option  -:  on  how  to  read
       (latitude,longitude,...) files.

REQUIRED ARGUMENTS

       table  One  or  more  ASCII (or binary, see -bi[ncols][type]) data table file(s) holding a number of data
              columns. If no tables are given then we read from standard input.

       -Erotfile
              Give file with rotation parameters. This file must contain one  record  for  each  rotation;  each
              record must be of the following format:

              lon lat tstart [tstop] angle [ khat a b c d e f g df ]

              where  tstart and tstop are in Myr and lon lat angle are in degrees. tstart and tstop are the ages
              of the old and young ends of a stage. If  tstop  is  not  present  in  the  record  then  a  total
              reconstruction  rotation  is expected and tstop is implicitly set to 0 and should not be specified
              for any of the records in the file. If a covariance matrix C for the rotation is available it must
              be specified in a format using the nine optional terms listed in brackets. Here, C = (g/khat)*[  a
              b  d; b c e; d e f ] which shows C made up of three row vectors. If the degrees of freedom (df) in
              fitting the rotation is 0 or not given it is set to 10000. Blank lines  and  records  whose  first
              column  contains  #  will  be ignored. You may prepend a leading + to the filename to indicate you
              wish to invert the rotations.   Alternatively,  give  the  filename  composed  of  two  plate  IDs
              separated  by  a hyphen (e.g., PAC-MBL) and we will instead extract that rotation from the GPlates
              rotation database. We return an error if the rotation cannot be found.

       -GCVAgrid
              Specify name for output grid file.

       -Ixinc[unit][=|+][/yinc[unit][=|+]]
              x_inc [and  optionally  y_inc]  is  the  grid  spacing.  Optionally,  append  a  suffix  modifier.
              Geographical (degrees) coordinates: Append m to indicate arc minutes or s to indicate arc seconds.
              If  one  of the units e, f, k, M, n or u is appended instead, the increment is assumed to be given
              in meter, foot, km, Mile, nautical mile or US survey foot, respectively, and will be converted  to
              the  equivalent  degrees longitude at the middle latitude of the region (the conversion depends on
              PROJ_ELLIPSOID). If /y_inc is given but set to 0 it will be reset equal  to  x_inc;  otherwise  it
              will  be  converted  to degrees latitude. All coordinates: If = is appended then the corresponding
              max x (east) or y (north) may be slightly adjusted to fit exactly the given increment [by  default
              the  increment  may  be  adjusted slightly to fit the given domain]. Finally, instead of giving an
              increment you may specify the number of nodes desired by  appending  +  to  the  supplied  integer
              argument;  the  increment  is  then  recalculated  from  the  number  of nodes and the domain. The
              resulting  increment  value  depends  on  whether  you  have  selected  a  gridline-registered  or
              pixel-registered  grid; see App-file-formats for details. Note: if -Rgrdfile is used then the grid
              spacing has already been initialized; use -I to override the values.

       -R[unit]west/east/south/north[/zmin/zmax][r]
              west, east, south, and north specify the region of interest, and you may specify them  in  decimal
              degrees  or  in  [+-]dd:mm[:ss.xxx][W|E|S|N]  format.  Append  r if lower left and upper right map
              coordinates are given instead of w/e/s/n. The two shorthands -Rg and -Rd stand for  global  domain
              (0/360 and -180/+180 in longitude respectively, with -90/+90 in latitude).  Alternatively for grid
              creation,  give  Rcodelon/lat/nx/ny, where code is a 2-character combination of L, C, R (for left,
              center, or right) and T, M, B for top, middle, or bottom. e.g., BL for lower left.  This indicates
              which point on a rectangular region the lon/lat coordinate refers to, and the grid  dimensions  nx
              and  ny  with  grid  spacings  via  -I is used to create the corresponding region.  Alternatively,
              specify the name of an existing grid file and the -R settings (and grid  spacing,  if  applicable)
              are  copied  from the grid. Using -Runit expects projected (Cartesian) coordinates compatible with
              chosen -J and we inversely  project  to  determine  actual  rectangular  geographic  region.   For
              perspective  view (-p), optionally append /zmin/zmax.  In case of perspective view (-p), a z-range
              (zmin, zmax) can be appended to indicate the third dimension. This needs  to  be  done  only  when
              using  the -Jz option, not when using only the -p option. In the latter case a perspective view of
              the plane is plotted, with no third dimension.

OPTIONAL ARGUMENTS

       -Dfactor
              Modify the sampling interval along flowlines. Default [0.5] gives approximately  2  points  within
              each grid box. Smaller factors gives higher resolutions at the expense of longer processing time.

       -Nupper_age
              Set the upper age to assign seamounts whose crustal age is unknown (i.e., NaN) [no upper age].

       -S     Normalize the resulting CVA grid to percentages of the CVA maximum.

       -T     Truncate seamount ages exceeding the upper age set with -N [no truncation].

       -V[level] (more ...)
              Select verbosity level [c].

       -bi[ncols][t] (more ...)
              Select native binary input. [Default is 5 input columns].

       -dinodata (more ...)
              Replace input columns that equal nodata with NaN.

       -V[level] (more ...)
              Select verbosity level [c].

       -icols[l][sscale][ooffset][,...] (more ...)
              Select input columns (0 is first column).

       -ocols[,...] (more ...)
              Select output columns (0 is first column).

       -r (more ...)
              Set pixel node registration [gridline].

       -:[i|o] (more ...)
              Swap 1st and 2nd column on input and/or output.

       -^ or just -
              Print a short message about the syntax of the command, then exits (NOTE: on Windows use just -).

       -+ or just +
              Print  an  extensive usage (help) message, including the explanation of any module-specific option
              (but not the GMT common options), then exits.

       -? or no arguments
              Print a complete usage (help) message, including the explanation of options, then exits.

       --version
              Print GMT version and exit.

       --show-datadir
              Print full path to GMT share directory and exit.

GEODETIC VERSUS GEOCENTRIC COORDIINATES

       All spherical rotations are applied to geocentric coordinates.  This means that incoming data points  and
       grids  are  considered  to  represent  geodetic  coordinates  and  must  first be converted to geocentric
       coordinates. Rotations are then applied, and  the  final  reconstructed  points  are  converted  back  to
       geodetic  coordinates.   This default behavior can be bypassed if the ellipsoid setting PROJ_ELLIPSOID is
       changed to Sphere.

EXAMPLES

       To create a CVA image from the Pacific (x,y,z,r,t) data in the file seamounts.d, using the  DC85.d  Euler
       poles, run

              gmt hotspotter seamounts.d -EDC85.d -GCVA.nc -R130/260/-66/60 -I10m -N145 -T -V

       This file can then be plotted with grdimage.

NOTES

       GMT  distributes  the  EarthByte  rotation  model  Global_EarthByte_230-0Ma_GK07_AREPS.rot.   To  use  an
       alternate rotation file, create an environmental parameters named GPLATES_ROTATIONS  that  points  to  an
       alternate rotation file.

SEE ALSO

       gmt, grdimage, grdrotater, grdspotter, project, mapproject, backtracker, originator

REFERENCES

       Wessel, P., 1999, "Hotspotting" tools released, EOS Trans. AGU, 80 (29), p. 319.

       Wessel,  P.,  2008,  Hotspotting: Principles and properties of a plate tectonic Hough transform, Geochem.
       Geophys. Geosyst. 9(Q08004): doi:10.1029/2008GC002058.

COPYRIGHT

       2015, P. Wessel, W. H. F. Smith, R. Scharroo, J. Luis, and F. Wobbe

5.2.1                                           January 28, 2016                                HOTSPOTTER(1gmt)