ANSI-C program: def_trans_pt.c
NAME
  def_trans_pt - Surface displacement map generation from unwrapped
  differential phase.
SYNOPSIS
  def_trans_pt <plist> <pmask>
  <pSLC_par> <pdef> <phgt> <pdef2>
  [mode]
| <plist> | (input) point list (int) | 
| <pmask> | (input) point data stack of mask values (uchar, set to - to accept all points) | 
| <SLC_par> | (input) ISP SLC/MLI parameter file of the reference SLC image (text) | 
| <pdef> | point data stack deformation rate along the line of sight (float) | 
| <phgt> | (input) point data stack of terrain heights (float) (enter - for none) | 
| <pdef2> | (output) equivelent vertical or horizontal deformation rate (binary) | 
| <mode> | displacement calculation mode: 0: vertical, +: increasing height (m) 1: horizontal, +: decreasing ground range (m) | 
EXAMPLE
  def_trans_pt pt pmsk1 19960421.slc.par pdef phgt pdef_vert
  1
Converts the LOS deformation rate to a vertical displacement
  rate map. The point list is pt and the point  mask is
  pmsk1
DESCRIPTION
  def_trans_pt converts
  the deformation rate along the line of sight (LOS) into the
  equivalent vertical or horizontal deformation rate. The nominal
  units are meters/year. The basic assumption is all the
  deformation is either vertical or horizontal. The observed LOS
  deformation rate is the component of this vertical or horizontal
  deformation along the LOS. The geometrical reference is chosen to
  be reference SLC.
To determine the equivalent deformation rate in the vertical direction mode 0 is selected. For horizontal deformation rates, mode 1 is selected. Positive signs corresponding to increasing surface height and negative signs to subsidence, def_trans_pt mode 0 is selected. Vertical displacement can often be assumed in the case of subsidence.
To map the equivalent horizontal displacement rate cin the
  ground range direction with a positive sign  corresponding
  to decreasing ground range, def_trans_pt mode 1 is selected.
  Note that the mapping of displacement rate along the terrain
  surface, as required in the mapping of glacier velocity, is not
  supported by def_trans_pt.
OPTIONS
  Terrain heights are required for the conversion of the
  deformation rate to the equivalent deformation rate in the
  vertical or horizontal direction. As an option the height point
  data does not need to be entered and a surface reference height
  0f 0.0 m is used for the conversion. The effect of the terrain
  height on the result may in many cases be neglected in comparison
  to other error sources.
SEE ALSO
  ipta.h.