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authorKristian Evers <kristianevers@gmail.com>2018-02-28 21:55:24 +0100
committerKristian Evers <kristianevers@gmail.com>2018-02-28 21:58:08 +0100
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tree9bbec3c7ae8ca39d00f146e6a389cbfedf44550d /docs/source/htpd.rst
parentd905a1136b6941f211818156e6b154b06eadfcc0 (diff)
downloadPROJ-ad73427eb7a90f0b96a67a6c0b6c0892096850f5.tar.gz
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Add section on PROJ resource files to docs [skip ci]
Added new section on PROJ resource files to the top level of the documentation. Moved information on init-file from the 'usage' chapter to the new section. Also moved pages on grids and HTPD to the new resource files section. Finally links and information on the new regional datumgrids packages is added.
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-.. _htpd:
-
-================================================================================
-HTPD
-================================================================================
-
-.. contents:: Contents
- :depth: 2
- :backlinks: none
-
-This page documents use of the `crs2crs2grid.py` script and the HTDP
-(Horizontal Time Dependent Positioning) grid shift modelling program from
-NGS/NOAA to produce PROJ compatible grid shift files for fine grade
-conversions between various NAD83 epochs and WGS84. Traditionally PROJ has
-treated NAD83 and WGS84 as equivalent and failed to distinguish between
-different epochs or realizations of those datums. At the scales of much
-mapping this is adequate but as interest grows in high resolution imagery and
-other high resolution mapping this is inadequate. Also, as the North American
-crust drifts over time the displacement between NAD83 and WGS84 grows (more
-than one foot over the last two decades).
-
-Getting and building HTDP
---------------------------------------------------------------------------------
-
-The HTDP modelling program is in written FORTRAN. The source and documentation
-can be found on the HTDP page at http://www.ngs.noaa.gov/TOOLS/Htdp/Htdp.shtml
-
-On linux systems it will be necessary to install `gfortran` or some FORTRAN
-compiler. For ubuntu something like the following should work.
-
-::
-
- apt-get install gfortran
-
-To compile the program do something like the following to produce the binary "htdp" from the source code.
-
-::
-
- gfortran htdp.for -o htdp
-
-Getting crs2crs2grid.py
---------------------------------------------------------------------------------
-
-The `crs2crs2grid.py` script can be found at
-https://github.com/OSGeo/gdal/tree/trunk/gdal/swig/python/samples/crs2crs2grid.py
-
-It depends on having the GDAL Python bindings operational. If they are not
-available you will get an error something like the following:
-
-
-::
-
- Traceback (most recent call last):
- File "./crs2crs2grid.py", line 37, in <module>
- from osgeo import gdal, gdal_array, osr
- ImportError: No module named osgeo
-
-Usage
---------------------------------------------------------------------------------
-
-::
-
- crs2crs2grid.py
- <src_crs_id> <src_crs_date> <dst_crs_id> <dst_crs_year>
- [-griddef <ul_lon> <ul_lat> <ll_lon> <ll_lat> <lon_count> <lat_count>]
- [-htdp <path_to_exe>] [-wrkdir <dirpath>] [-kwf]
- -o <output_grid_name>
-
- -griddef: by default the following values for roughly the continental USA
- at a six minute step size are used:
- -127 50 -66 25 251 611
- -kwf: keep working files in the working directory for review.
-
-::
-
- crs2crs2grid.py 29 2002.0 8 2002.0 -o nad83_2002.ct2
-
-The goal of `crs2crs2grid.py` is to produce a grid shift file for a designated
-region. The region is defined using the `-griddef` switch. When missing a
-continental US region is used. The script creates a set of sample points for
-the grid definition, runs the "htdp" program against it and then parses the
-resulting points and computes a point by point shift to encode into the final
-grid shift file. By default it is assumed the `htdp` program will be in the
-executable path. If not, please provide the path to the executable using the
-`-htdp` switch.
-
-The `htdp` program supports transformations between many CRSes and for each (or
-most?) of them you need to provide a date at which the CRS is fixed. The full
-set of CRS Ids available in the HTDP program are:
-
-::
-
- 1...NAD_83(2011) (North America tectonic plate fixed)
- 29...NAD_83(CORS96) (NAD_83(2011) will be used)
- 30...NAD_83(2007) (NAD_83(2011) will be used)
- 2...NAD_83(PA11) (Pacific tectonic plate fixed)
- 31...NAD_83(PACP00) (NAD 83(PA11) will be used)
- 3...NAD_83(MA11) (Mariana tectonic plate fixed)
- 32...NAD_83(MARP00) (NAD_83(MA11) will be used)
-
- 4...WGS_72 16...ITRF92
- 5...WGS_84(transit) = NAD_83(2011) 17...ITRF93
- 6...WGS_84(G730) = ITRF92 18...ITRF94 = ITRF96
- 7...WGS_84(G873) = ITRF96 19...ITRF96
- 8...WGS_84(G1150) = ITRF2000 20...ITRF97
- 9...PNEOS_90 = ITRF90 21...IGS97 = ITRF97
- 10...NEOS_90 = ITRF90 22...ITRF2000
- 11...SIO/MIT_92 = ITRF91 23...IGS00 = ITRF2000
- 12...ITRF88 24...IGb00 = ITRF2000
- 13...ITRF89 25...ITRF2005
- 14...ITRF90 26...IGS05 = ITRF2005
- 15...ITRF91 27...ITRF2008
- 28...IGS08 = ITRF2008
-
-The typical use case is mapping from NAD83 on a particular date to WGS84 on
-some date. In this case the source CRS Id "29" (NAD_83(CORS96)) and the
-destination CRS Id is "8 (WGS_84(G1150)). It is also necessary to select the
-source and destination date (epoch). For example:
-
-::
-
- crs2crs2grid.py 29 2002.0 8 2002.0 -o nad83_2002.ct2
-
-The output is a CTable2 format grid shift file suitable for use with PROJ
-(4.8.0 or newer). It might be utilized something like:
-
-
-::
-
- cs2cs +proj=latlong +ellps=GRS80 +nadgrids=./nad83_2002.ct2 +to +proj=latlong +datum=WGS84
-
-See Also
---------------------------------------------------------------------------------
-
-* http://www.ngs.noaa.gov/TOOLS/Htdp/Htdp.shtml - NGS/NOAA page about the HTDP
- model and program. Source for the HTDP program can be downloaded from here.