NAME
surface - adjustable tension continuous curvature surface gridding algorithmSYNOPSIS
surface [ xyzfile ] -Goutputfile.grd -Ix_inc[ m|c][/y_inc[m|c]] -Rwest/east/south/north[ r] [ -Aaspect_ratio ] [ -Cconvergence_limit ] [ -H[ nrec] ] [ -L ] [ -Lllower ] [ -Lu upper ] [ -Nmax_iterations ] [ -Q ] [ -Ssearch_radius[m] ] [ -Ttension_factor[ib] ] [ -V[l] ] [ -Z over-relaxation_factor ] [ -: ] [ -bi[s][ n] ]DESCRIPTION
surface reads randomly-spaced (x,y,z) triples from standard input [or xyzfile] and produces a binary grdfile of gridded values z(x,y) by solving:(1 - T) * L (L (z)) + T * L (z) = 0
- xyzfile
- 3 column ASCII file [or binary, see -b] holding (x,y,z) data values. If no file is specified, surface will read from standard input.
- -G
- Output file name. Output is a binary 2-D .grd file.
- -I
- x_inc [and optionally y_inc] is the grid spacing. Append m to indicate minutes or c to indicate seconds.
- -R
- west, east, south, and north specify the Region of interest. To specify boundaries in degrees and minutes [and seconds], use the dd:mm[:ss] format. Append r if lower left and upper right map coordinates are given instead of wesn.
OPTIONS
- -A
- Aspect ratio. If desired, grid anisotropy can be added to the equations. Enter aspect_ratio, where dy = dx / aspect_ratio relates the grid dimensions. [Default = 1 assumes isotropic grid.]
- -C
- Convergence limit. Iteration is assumed to have converged when the maximum absolute change in any grid value is less than convergence_limit. (Units same as data z units). [Default is scaled to 0.1 percent of typical gradient in input data.]
- -H
- Input file(s) has Header record(s). Number of header records can be changed by editing your .gmtdefaults file. If used, GMT default is 1 header record. Not used with binary data.
- -L
- Without any modifier, this option indicates that x is longitude and may be periodic in 360 degrees. With optional arguments it will instead impose limits on the output solution. llower sets the lower bound. lower can be the name of a grdfile with lower bound values, a fixed value, d to set to minimum input value, or u for unconstrained [Default]. uupper sets the upper bound and can be the name of a grdfile with upper bound values, a fixed value, d to set to maximum input value, or u for unconstrained [Default].
- -N
- Number of iterations. Iteration will cease when convergence_limit is reached or when number of iterations reaches max_iterations. [Default is 250.]
- -Q
- Suggest grid dimensions which have a highly composite greatest common factor. This allows surface to use several intermediate steps in the solution, yielding faster run times and better results. The sizes suggested by -Q can be achieved by altering -R and/or -I. You can recover the -R and -I you want later by using grdsample or grdcut on the output of surface.
- -S
- Search radius. Enter search_radius in same units as x,y data; append m to indicate minutes. This is used to initialize the grid before the first iteration; it is not worth the time unless the grid lattice is prime and cannot have regional stages. [Default = 0.0 and no search is made.]
- -T
- Tension factor[s]. These must be between 0 and 1. Tension may be used in the interior solution (above equation, where it suppresses spurious oscillations) and in the boundary conditions (where it tends to flatten the solution approaching the edges). Using zero for both values results in a minimum curvature surface with free edges, i.e. a natural bicubic spline. Use -Ttension_factori to set interior tension, and -Ttension_factorb to set boundary tension. If you do not append i or b, both will be set to the same value. [Default = 0 for both gives minimum curvature solution.]
- -V
- Selects verbose mode, which will send progress reports to stderr [Default runs "silently"]. -Vl will report the convergence after each iteration; -V will report only after each regional grid is converged.
- -Z
- Over-relaxation factor. This parameter is used to accelerate the convergence; it is a number between 1 and 2. A value of 1 iterates the equations exactly, and will always assure stable convergence. Larger values overestimate the incremental changes during convergence, and will reach a solution more rapidly but may become unstable. If you use a large value for this factor, it is a good idea to monitor each iteration with the -Vl option. [Default = 1.4 converges quickly and is almost always stable.]
- -:
- Toggles between (longitude,latitude) and (latitude,longitude) input/output. [Default is (longitude,latitude)]. Applies to geographic coordinates only.
- -bi
- Selects binary input. Append s for single precision [Default is double]. Append n for the number of columns in the binary file(s). [Default is 3 input columns].
EXAMPLES
To grid 5 by 5 minute gravity block means from the ASCII data in hawaii_5x5.xyg, using a tension_factor = 0.25, a convergence_limit = 0.1 milligal, writing the result to a file called hawaii_grd.grd, and monitoring each iteration, try:BUGS
surface will complain when more than one data point is found for any node and suggest that you run blockmean, blockmedian, or blockmode first. If you did run blockm* and still get this message it usually means that your grid spacing is so small that you need more decimals in the output format used by blockm*. You may specify more decimal places by editing the parameter D_FORMAT in your .gmtdefaults file prior to running blockm*, or choose binary input and/or output using single or double precision storage.SEE ALSO
blockmean(1gmt), blockmedian(1gmt), blockmode(1gmt), gmt(1gmt), nearneighbor(1gmt), triangulate(1gmt)REFERENCES
Smith, W. H. F, and P. Wessel, 1990, Gridding with continuous curvature splines in tension, Geophysics, 55, 293-305.| 1 Jan 2004 |