|
8 | 8 |
|
9 | 9 | Perform datum shifts by means of a deformation/velocity model.
|
10 | 10 |
|
11 |
| - X_out = X_in + (T_ct - T_obs)*DX |
12 |
| - Y_out = Y_in + (T_ct - T_obs)*DY |
13 |
| - Z_out = Z_in + (T_ct - T_obs)*DZ |
14 |
| -
|
| 11 | + X_out = X_in + (T_obs - T_epoch) * DX |
| 12 | + Y_out = Y_in + (T_obs - T_epoch) * DY |
| 13 | + Z_out = Z_in + (T_obs - T_epoch) * DZ |
15 | 14 |
|
16 | 15 | The deformation operation takes cartesian coordinates as input and
|
17 | 16 | returns cartesian coordinates as well.
|
18 | 17 |
|
19 | 18 | Corrections in the gridded model are in east, north, up (ENU) space.
|
20 |
| -Hence the input coordinates needs to be converted to ENU-space when |
| 19 | +Hence the input coordinates need to be converted to ENU-space when |
21 | 20 | searching for corrections in the grid. The corrections are then converted
|
22 | 21 | to cartesian PJ_XYZ-space and applied to the input coordinates (also in
|
23 | 22 | cartesian space).
|
24 | 23 |
|
25 |
| -A full deformation model is described by two grids, one for the horizontal |
26 |
| -components and one for the vertical component. The horizontal grid is |
27 |
| -stored in CTable/CTable2 and the vertical grid is stored in the GTX |
28 |
| -format. The NTv2 format should not be used for this purpose since grid- |
29 |
| -values are scaled upon reading. Both grids are expected to contain |
30 |
| -grid-values in units of mm/year in ENU-space. |
| 24 | +A full deformation model is preferably represented as a 3 channel Geodetic |
| 25 | +TIFF Grid, but was historically described by a set of two grids: One for |
| 26 | +the horizontal components and one for the vertical component. |
| 27 | +
|
| 28 | +The east and north components are (were) stored using the CTable/CTable2 |
| 29 | +format, up component is (was) stored in the GTX format. Both grids are |
| 30 | +(were) expected to contain grid-values in units of mm/year in ENU-space. |
31 | 31 |
|
32 | 32 | ************************************************************************
|
33 | 33 | * Copyright (c) 2017, Kristian Evers
|
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