Coverage for pygeodesy/trf.py : 98%

Hot-keys on this page
r m x p toggle line displays
j k next/prev highlighted chunk
0 (zero) top of page
1 (one) first highlighted chunk
# -*- coding: utf-8 -*-
Transcribed from I{Chris Veness'} (C) 2006-2019 JavaScript originals U{latlon-ellipsoidal-referenceframe.js<https://GitHub.com/chrisveness/geodesy/blob/master/ latlon-ellipsoidal-referenceframe.js>} and U{latlon-ellipsoidal-referenceframe-txparams.js <https://GitHub.com/chrisveness/geodesy/blob/master/latlon-ellipsoidal-referenceframe-txparams.js>}.
Modern geodetic reference frames: a latitude/longitude point defines a geographic location on, above or below the earth’s surface, measured in degrees from the equator and the U{International Reference Meridian<https://WikiPedia.org/wiki/IERS_Reference_Meridian>} (IRM) and metres above the ellipsoid within a given I{Terrestrial Reference Frame} at a given I{epoch}.
This is scratching the surface of complexities involved in high precision geodesy, but may be of interest and/or value to those with less demanding requirements. More information U{here <https://www.Movable-Type.co.UK/scripts/geodesy-library.html>} and U{here <https://www.Movable-Type.co.UK/scripts/geodesy-library.html#latlon-ellipsoidal-referenceframe>}.
Note that I{ITRF solutions} do not directly use an ellipsoid, but are specified by Cartesian coordinates. The GRS80 ellipsoid is recommended for transformations to geographical coordinates.
Note WGS84(G730/G873/G1150) are coincident with ITRF at 10-centimetre level, see also U{here <ftp://ITRF.ENSG.IGN.FR/pub/itrf/WGS84.TXT>}. WGS84(G1674) and ITRF20014 / ITRF2008 ‘are likely to agree at the centimeter level’, see also U{QPS/QINSy<https://Confluence.QPS.NL/qinsy/ en/how-to-deal-with-etrs89-datum-and-time-dependent-transformation-parameters-45353274.html>}.
@var RefFrames.ETRF2000: RefFrame(name='ETRF2000', epoch=2005.0, ellipsoid=Ellipsoid(name='GRS80') @var RefFrames.GDA94: RefFrame(name='GDA94', epoch=1994.0, ellipsoid=Ellipsoid(name='GRS80') @var RefFrames.ITRF2000: RefFrame(name='ITRF2000', epoch=1997.0, ellipsoid=Ellipsoid(name='GRS80') @var RefFrames.ITRF2005: RefFrame(name='ITRF2005', epoch=2000.0, ellipsoid=Ellipsoid(name='GRS80') @var RefFrames.ITRF2008: RefFrame(name='ITRF2008', epoch=2005.0, ellipsoid=Ellipsoid(name='GRS80') @var RefFrames.ITRF2014: RefFrame(name='ITRF2014', epoch=2010.0, ellipsoid=Ellipsoid(name='GRS80') @var RefFrames.ITRF91: RefFrame(name='ITRF91', epoch=1988.0, ellipsoid=Ellipsoid(name='GRS80') @var RefFrames.ITRF93: RefFrame(name='ITRF93', epoch=1988.0, ellipsoid=Ellipsoid(name='GRS80') @var RefFrames.NAD83: RefFrame(name='NAD83', epoch=1997.0, ellipsoid=Ellipsoid(name='GRS80') @var RefFrames.WGS84g1150: RefFrame(name='WGS84g1150', epoch=2001.0, ellipsoid=Ellipsoid(name='WGS84') @var RefFrames.WGS84g1674: RefFrame(name='WGS84g1674', epoch=2005.0, ellipsoid=Ellipsoid(name='WGS84') @var RefFrames.WGS84g1762: RefFrame(name='WGS84g1762', epoch=2005.0, ellipsoid=Ellipsoid(name='WGS84') '''
_epoch_, _float as _F, _floatuple as _T, \ _name_, _no_conversion_, _0_0 _NamedEnum, _NamedEnumItem
'''Single-instance strings. '''
'''Terrestrial Reference Frame (TRF) parameters. '''
'''New L{RefFrame}.
@arg epoch: Epoch, a fractional calendar year (C{scalar} or C{str}). @arg ellipsoid: The ellipsoid (L{Ellipsoid}, L{Ellipsoid2}, L{datum} or L{a_f2Tuple}). @kwarg name: Optional, unique name (C{str}).
@raise NameError: A L{RefFrame} with that B{C{name}} already exists.
@raise TRFError: Invalid B{C{epoch}}.
@raise TypeError: Invalid B{C{ellipsoid}}. '''
'''Get this reference frame's ellipsoid (L{Ellipsoid} or L{Ellipsoid2}). '''
'''Get this reference frame's epoch (C{Epoch}). '''
'''Return this reference frame as a text string.
@return: This L{RefFrame}'s attributes (C{str}). ''' '%s=%s' % (_epoch_, self.epoch), '%s=%s(%s=%r)' % (_ellipsoid_, classname(e), _name_, e.name))
# <https://GitHub.com/chrisveness/geodesy/blob/master/latlon-ellipsoidal-referenceframe.js> # ITRF2014AU = RefFrame(_F(2020), Ellipsoids.GRS80, _S.ITRF2014AU), ITRF2014 = RefFrame(_F(2010), Ellipsoids.GRS80, _S.ITRF2014), ITRF2008 = RefFrame(_F(2005), Ellipsoids.GRS80, _S.ITRF2008), ITRF2005 = RefFrame(_F(2000), Ellipsoids.GRS80, _S.ITRF2005), ITRF2000 = RefFrame(_F(1997), Ellipsoids.GRS80, _S.ITRF2000), ITRF93 = RefFrame(_F(1988), Ellipsoids.GRS80, _S.ITRF93), ITRF91 = RefFrame(_F(1988), Ellipsoids.GRS80, _S.ITRF91), WGS84g1762 = RefFrame(_F(2005), Ellipsoids.WGS84, _S.WGS84g1762), WGS84g1674 = RefFrame(_F(2005), Ellipsoids.WGS84, _S.WGS84g1674), WGS84g1150 = RefFrame(_F(2001), Ellipsoids.WGS84, _S.WGS84g1150), ETRF2000 = RefFrame(_F(2005), Ellipsoids.GRS80, _S.ETRF2000), # ETRF2000(R08) NAD83 = RefFrame(_F(1997), Ellipsoids.GRS80, _S.NAD83), # CORS96 GDA94 = RefFrame(_F(1994), Ellipsoids.GRS80, _S.GDA94))
'''Return the reference frame C{epoch} for a calendar day.
@arg year: Year of the date (C{scalar}). @arg month: Month in the B{C{year}} (C{scalar}, 1..12). @arg day: Day in the B{C{month}} (C{scalar}, 1..31).
@return: Epoch, the fractional year (C{float}).
@raise TRFError: Invalid B{C{year}}, B{C{month}} or B{C{day}}.
@note: Any B{C{year}} is considered a leap year, i.e. having 29 days in February. '''
t = NN # _invalid_ raise TRFError(year=year, month=month, day=day, txt=t)
'''Return the date for a reference frame C{epoch}.
@arg epoch: Fractional year (C{scalar}).
@return: 3-Tuple C{(year, month, day)}.
@raise TRFError: Invalid B{C{epoch}}.
@note: Any B{C{year}} is considered a leap year, i.e. having 29 days in February. ''' else:
# TRF conversions specified as 7-parameter Helmert transforms and an epoch. Most # from U{Transformation Parameters<http://ITRF.IGN.FR/trans_para.php>}, more at U{QPS # <https://Confluence.QPS.NL/qinsy/files/en/29856813/45482834/2/1453459502000/ITRF_Transformation_Parameters.xlsx>}. # see U{Transformation Parameters ITRF2014<http://ITRF.IGN.FR/doc_ITRF/Transfo-ITRF2014_ITRFs.txt>} (_S.ITRF2014, _S.ITRF2008): _D(epoch=_F(2010), # <http://ITRF.ENSG.IGN.FR/ITRF_solutions/2014/tp_14-08.php> xform=_T( 1.6, 1.9, 2.4, -0.02, 0.0, 0.0, 0.0), rates=_T( 0.0, 0.0, -0.1, 0.03, 0.0, 0.0, 0.0)), (_S.ITRF2014, _S.ITRF2005): _D(epoch=_F(2010), xform=_T( 2.6, 1.0, -2.3, 0.92, 0.0, 0.0, 0.0), rates=_T( 0.3, 0.0, -0.1, 0.03, 0.0, 0.0, 0.0)), (_S.ITRF2014, _S.ITRF2000): _D(epoch=_F(2010), xform=_T( 0.7, 1.2, -26.1, 2.12, 0.0, 0.0, 0.0), rates=_T( 0.1, 0.1, -1.9, 0.11, 0.0, 0.0, 0.0)), (_S.ITRF2014, _S.ITRF97): _D(epoch=_F(2010), xform=_T( 7.4, -0.5, -62.8, 3.8, 0.0, 0.0, 0.26), rates=_T( 0.1, -0.5, -3.3, 0.12, 0.0, 0.0, 0.02)), (_S.ITRF2014, _S.ITRF96): _D(epoch=_F(2010), xform=_T( 7.4, -0.5, -62.8, 3.8, 0.0, 0.0, 0.26), rates=_T( 0.1, -0.5, -3.3, 0.12, 0.0, 0.0, 0.02)), (_S.ITRF2014, _S.ITRF94): _D(epoch=_F(2010), xform=_T( 7.4, -0.5, -62.8, 3.8, 0.0, 0.0, 0.26), rates=_T( 0.1, -0.5, -3.3, 0.12, 0.0, 0.0, 0.02)), (_S.ITRF2014, _S.ITRF93): _D(epoch=_F(2010), xform=_T(-50.4, 3.3, -60.2, 4.29, -2.81, -3.38, 0.4), rates=_T( -2.8, -0.1, -2.5, 0.12, -0.11, -0.19, 0.07)), (_S.ITRF2014, _S.ITRF92): _D(epoch=_F(2010), xform=_T( 15.4, 1.5, -70.8, 3.09, 0.0, 0.0, 0.26), rates=_T( 0.1, -0.5, -3.3, 0.12, 0.0, 0.0, 0.02)), (_S.ITRF2014, _S.ITRF91): _D(epoch=_F(2010), xform=_T( 27.4, 15.5, -76.8, 4.49, 0.0, 0.0, 0.26), rates=_T( 0.1, -0.5, -3.3, 0.12, 0.0, 0.0, 0.02)), (_S.ITRF2014, _S.ITRF90): _D(epoch=_F(2010), xform=_T( 25.4, 11.5, -92.8, 4.79, 0.0, 0.0, 0.26), rates=_T( 0.1, -0.5, -3.3, 0.12, 0.0, 0.0, 0.02)), (_S.ITRF2014, _S.ITRF89): _D(epoch=_F(2010), xform=_T( 30.4, 35.5, -130.8, 8.19, 0.0, 0.0, 0.26), rates=_T( 0.1, -0.5, -3.3, 0.12, 0.0, 0.0, 0.02)), (_S.ITRF2014, _S.ITRF88): _D(epoch=_F(2010), xform=_T( 25.4, -0.5, -154.8, 11.29, 0.1, 0.0, 0.26), rates=_T( 0.1, -0.5, -3.3, 0.12, 0.0, 0.0, 0.02)),
# see U{Transformation Parameters ITRF2008<http://ITRF.IGN.FR/doc_ITRF/Transfo-ITRF2008_ITRFs.txt>} # (_S.ITRF2008, _S.ITRF2005): _D(epoch=_F(2005), # <http://ITRF.ENSG.IGN.FR/ITRF_solutions/2008/tp_08-05.php> # xform=_T( -0.5, -0.9, -4.7, 0.94, 0.0, 0.0, 0.0), # rates=_T( 0.3, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0)), (_S.ITRF2008, _S.ITRF2005): _D(epoch=_F(2000), xform=_T( -2.0, -0.9, -4.7, 0.94, 0.0, 0.0, 0.0), rates=_T( 0.3, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0)), (_S.ITRF2008, _S.ITRF2000): _D(epoch=_F(2000), xform=_T( -1.9, -1.7, -10.5, 1.34, 0.0, 0.0, 0.0), rates=_T( 0.1, 0.1, -1.8, 0.08, 0.0, 0.0, 0.0)), (_S.ITRF2008, _S.ITRF97): _D(epoch=_F(2000), xform=_T( 4.8, 2.6, -33.2, 2.92, 0.0, 0.0, 0.06), rates=_T( 0.1, -0.5, -3.2, 0.09, 0.0, 0.0, 0.02)), (_S.ITRF2008, _S.ITRF96): _D(epoch=_F(2000), xform=_T( 4.8, 2.6, -33.2, 2.92, 0.0, 0.0, 0.06), rates=_T( 0.1, -0.5, -3.2, 0.09, 0.0, 0.0, 0.02)), (_S.ITRF2008, _S.ITRF94): _D(epoch=_F(2000), xform=_T( 4.8, 2.6, -33.2, 2.92, 0.0, 0.0, 0.06), rates=_T( 0.1, -0.5, -3.2, 0.09, 0.0, 0.0, 0.02)), (_S.ITRF2008, _S.ITRF93): _D(epoch=_F(2000), xform=_T(-24.0, 2.4, -38.6, 3.41, -1.71, -1.48, -0.3), rates=_T( -2.8, -0.1, -2.4, 0.09, -0.11, -0.19, 0.07)), (_S.ITRF2008, _S.ITRF92): _D(epoch=_F(2000), xform=_T( 12.8, 4.6, -41.2, 2.21, 0.0, 0.0, 0.06), rates=_T( 0.1, -0.5, -3.2, 0.09, 0.0, 0.0, 0.02)), (_S.ITRF2008, _S.ITRF91): _D(epoch=_F(2000), xform=_T( 24.8, 18.6, -47.2, 3.61, 0.0, 0.0, 0.06), rates=_T( 0.1, -0.5, -3.2, 0.09, 0.0, 0.0, 0.02)), (_S.ITRF2008, _S.ITRF90): _D(epoch=_F(2000), xform=_T( 22.8, 14.6, -63.2, 3.91, 0.0, 0.0, 0.06), rates=_T( 0.1, -0.5, -3.2, 0.09, 0.0, 0.0, 0.02)), (_S.ITRF2008, _S.ITRF89): _D(epoch=_F(2000), xform=_T( 27.8, 38.6, -101.2, 7.31, 0.0, 0.0, 0.06), rates=_T( 0.1, -0.5, -3.2, 0.09, 0.0, 0.0, 0.02)), (_S.ITRF2008, _S.ITRF88): _D(epoch=_F(2000), xform=_T( 22.8, 2.6, -125.2, 10.41, 0.1, 0.0, 0.06), rates=_T( 0.1, -0.5, -3.2, 0.09, 0.0, 0.0, 0.02)),
(_S.ITRF2005, _S.ITRF2000): _D(epoch=_F(2000), # <http://ITRF.ENSG.IGN.FR/ITRF_solutions/2005/tp_05-00.php> xform=_T( 0.1, -0.8, -5.8, 0.4, 0.0, 0.0, 0.0), rates=_T( -0.2, 0.1, -1.8, 0.08, 0.0, 0.0, 0.0)),
(_S.ITRF2000, _S.ITRF97): _D(epoch=_F(1997), xform=_T( 0.67, 0.61, -1.85, 1.55, 0.0, 0.0, 0.0), rates=_T( 0.0, -0.06, -0.14, 0.01, 0.0, 0.0, 0.02)), (_S.ITRF2000, _S.ITRF96): _D(epoch=_F(1997), xform=_T( 0.67, 0.61, -1.85, 1.55, 0.0, 0.0, 0.0), rates=_T( 0.0, -0.06, -0.14, 0.01, 0.0, 0.0, 0.02)), (_S.ITRF2000, _S.ITRF94): _D(epoch=_F(1997), xform=_T( 0.67, 0.61, -1.85, 1.55, 0.0, 0.0, 0.0), rates=_T( 0.0, -0.06, -0.14, 0.01, 0.0, 0.0, 0.02)), (_S.ITRF2000, _S.ITRF93): _D(epoch=_F(1988), xform=_T( 12.7, 6.5, -20.9, 1.95, -0.39, 0.8, -1.14), rates=_T( -2.9, -0.2, -0.6, 0.01, -0.11, -0.19, 0.07)), (_S.ITRF2000, _S.ITRF92): _D(epoch=_F(1988), xform=_T( 1.47, 1.35, -1.39, 0.75, 0.0, 0.0, -0.18), rates=_T( 0.0, -0.06, -0.14, 0.01, 0.0, 0.0, 0.02)), (_S.ITRF2000, _S.ITRF91): _D(epoch=_F(1988), xform=_T( 26.7, 27.5, -19.9, 2.15, 0.0, 0.0, -0.18), rates=_T( 0.0, -0.6, -1.4, 0.01, 0.0, 0.0, 0.02)), (_S.ITRF2000, _S.ITRF90): _D(epoch=_F(1988), xform=_T( 2.47, 2.35, -3.59, 2.45, 0.0, 0.0, -0.18), rates=_T( 0.0, -0.06, -0.14, 0.01, 0.0, 0.0, 0.02)), (_S.ITRF2000, _S.ITRF89): _D(epoch=_F(1988), xform=_T( 2.97, 4.75, -7.39, 5.85, 0.0, 0.0, -0.18), rates=_T( 0.0, -0.06, -0.14, 0.01, 0.0, 0.0, 0.02)), (_S.ITRF2000, _S.ITRF88): _D(epoch=_F(1988), xform=_T( 2.47, 1.15, -9.79, 8.95, 0.1, 0.0, -0.18), rates=_T( 0.0, -0.06, -0.14, 0.01, 0.0, 0.0, 0.02)),
# see U{Boucher, C. & Altamimi, Z. "Memo: Specifications for reference frame fixing in the # analysis of a EUREF GPS campaign" (2011) <https://ETRS89.ENSG.IGN.FR/memo-V8.pdf>} and # Altamimi, Z. U{"Key results of ITRF2014 and implication to ETRS89 realization", EUREF2016 # <https://www.EUREF.EU/symposia/2016SanSebastian/01-02-Altamimi.pdf>}. (_S.ITRF2014, _S.ETRF2000): _D(epoch=_F(2000), xform=_T( 53.7, 51.2, -55.1, 1.02, 0.891, 5.39, -8.712), rates=_T( 0.1, 0.1, -1.9, 0.11, 0.081, 0.49, -0.792)), (_S.ITRF2008, _S.ETRF2000): _D(epoch=_F(2000), xform=_T( 52.1, 49.3, -58.5, 1.34, 0.891, 5.39, -8.712), rates=_T( 0.1, 0.1, -1.8, 0.08, 0.081, 0.49, -0.792)), (_S.ITRF2005, _S.ETRF2000): _D(epoch=_F(2000), xform=_T( 54.1, 50.2, -53.8, 0.4, 0.891, 5.39, -8.712), rates=_T( -0.2, 0.1, -1.8, 0.08, 0.081, 0.49, -0.792)), (_S.ITRF2000, _S.ETRF2000): _D(epoch=_F(2000), xform=_T( 54.0, 51.0, -48.0, 0.0, 0.891, 5.39, -8.712), rates=_T( 0.0, 0.0, 0.0, 0.0, 0.081, 0.49, -0.792)),
# see U{Solar, T. & Snay, R.A. "Transforming Positions and Velocities between the # International Terrestrial Reference Frame of 2000 and North American Datum of 1983" # (2004)<https://www.NGS.NOAA.gov/CORS/Articles/SolerSnayASCE.pdf>} (_S.ITRF2000, _S.NAD83): _D(epoch=_F(1997), # note NAD83(CORS96) xform=_T(995.6, -1901.3, -521.5, 0.62, 25.915, 9.426, 11.599), rates=_T( 0.7, -0.7, 0.5, -0.18, 0.067, -0.757, -0.051)),
# see Table 2 in U{Dawson, J. & Woods, A. "ITRF to GDA94 coordinate transformations", Journal of # Applied Geodesy 4 (2010), 189-199<https://www.ResearchGate.net/publication/258401581_ITRF_to_GDA94_coordinate_transformations>} # (note, sign of rotations for GDA94 reversed as "Australia assumes rotation to be of coordinate # axes" rather than the more conventional "position around the coordinate axes") (_S.ITRF2008, _S.GDA94): _D(epoch=_F(1994), xform=_T(-84.68, -19.42, 32.01, 9.71, -0.4254, 2.2578, 2.4015), rates=_T( 1.42, 1.34, 0.9, 0.109, 1.5461, 1.182, 1.1551)), (_S.ITRF2005, _S.GDA94): _D(epoch=_F(1994), xform=_T(-79.73, -6.86, 38.03, 6.636, 0.0351, -2.1211, -2.1411), rates=_T( 2.25, -0.62, -0.56, 0.294, -1.4707, -1.1443, -1.1701)), (_S.ITRF2000, _S.GDA94): _D(epoch=_F(1994), xform=_T(-45.91, -29.85, -20.37, 7.07, -1.6705, 0.4594, 1.9356), rates=_T( -4.66, 3.55, 11.24, 0.249, 1.7454, 1.4868, 1.224)), }
'''(INTERNAL) Find a trf* "in between" C{n1} and C{n2}. '''
'''(INTERNAL) Get 0, 1 or 2 Helmert C{Transforms} to convert reference frame C{rf} observed at C{epoch} into C{rf2}. ''' or (n2.startswith(_S.ITRF) and n1.startswith(_S.WGS84)):
_2Transform((n, n2), epoch, _Forward))
_2Transform((n2, n), epoch, _Reverse))
t = '%s %r to %r' % (RefFrame.__name__, n1, n2) raise TRFError(_no_conversion_, txt=t)
'''(INTERNAL) Combine a 14-element Helmert C{trfX} and C{d_epoch} into a single 7-element C{Transform}. ''' n, x, r in zip(_trfNs, X.xform, X.rates))
if __name__ == '__main__':
for m in range(1, 13): y, d = 2020, _mDays[m] e = date2epoch(y, m, d) print('%s(%d, %d, %d) %.3F' % (date2epoch.__name__, y, m, d, e))
# __doc__ of this file t = [''] + repr(RefFrames).split('\n') print('\n@var '.join(i.strip(',') for i in t))
# **) MIT License # # Copyright (C) 2016-2020 -- mrJean1 at Gmail -- All Rights Reserved. # # Permission is hereby granted, free of charge, to any person obtaining a # copy of this software and associated documentation files (the "Software"), # to deal in the Software without restriction, including without limitation # the rights to use, copy, modify, merge, publish, distribute, sublicense, # and/or sell copies of the Software, and to permit persons to whom the # Software is furnished to do so, subject to the following conditions: # # The above copyright notice and this permission notice shall be included # in all copies or substantial portions of the Software. # # THE SOFTWARE IS PROVIDED "AS IS", WITHOUT WARRANTY OF ANY KIND, EXPRESS # OR IMPLIED, INCLUDING BUT NOT LIMITED TO THE WARRANTIES OF MERCHANTABILITY, # FITNESS FOR A PARTICULAR PURPOSE AND NONINFRINGEMENT. IN NO EVENT SHALL # THE AUTHORS OR COPYRIGHT HOLDERS BE LIABLE FOR ANY CLAIM, DAMAGES OR # OTHER LIABILITY, WHETHER IN AN ACTION OF CONTRACT, TORT OR OTHERWISE, # ARISING FROM, OUT OF OR IN CONNECTION WITH THE SOFTWARE OR THE USE OR # OTHER DEALINGS IN THE SOFTWARE.
# % python -m pygeodesy.trf # len(_trfFs) 216 / len(_trfXs) 627: 34.4% # # date2epoch(2020, 1, 31) 2020.085 # date2epoch(2020, 2, 29) 2020.164 # date2epoch(2020, 3, 31) 2020.249 # date2epoch(2020, 4, 30) 2020.331 # date2epoch(2020, 5, 31) 2020.415 # date2epoch(2020, 6, 30) 2020.497 # date2epoch(2020, 7, 31) 2020.582 # date2epoch(2020, 8, 31) 2020.667 # date2epoch(2020, 9, 30) 2020.749 # date2epoch(2020, 10, 31) 2020.833 # date2epoch(2020, 11, 30) 2020.915 # date2epoch(2020, 12, 31) 2021.000 |