[Proj] Is egm08_25.gtx misplaced half a pixel?
Mikael Rittri
Mikael.Rittri at carmenta.com
Wed Oct 5 06:23:29 PDT 2011
Hello,
I have tried to use the geoid height file
http://download.osgeo.org/proj/vdatum/egm08_25/egm08_25.gtx,
which is discussed here:
http://trac.osgeo.org/proj/wiki/VerticalDatums
But I am beginning to think that the file is misaligned
(well, at least if ones uses GDAL 1.8 or later to read it).
>From gdalinfo (version 1.8.1), I get
Origin = (-180.041666666666660,90.041666666666686)
Pixel Size = (0.041666666666667,-0.041666666666667)
But I think the correct origin of the data is really
(-180.020833333333333,90.020833333333333)
that is, half a pixel farther east and south.
I suspect this may be caused by the nasty AREA_OR_POINT issue.
The file is dated 3 Sep 2010, so I guess it was created before
GDAL 1.8, when the semantics of AREA_OR_POINT = POINT changed.
http://trac.osgeo.org/gdal/wiki/rfc33_gtiff_pixelispoint
Or maybe the cause is something else.
Some evidence: I have used the gtx file to look up the geoid
height (using a Carmenta Engine version that uses GDAL 1.8.1),
at a position where the geoid slopes towards southeast,
145dE 13dN
and I found the value 44.925678 m.
But according to Charles Karney's online geoid calculator
http://geographiclib.sourceforge.net/cgi-bin/GeoidEval
the value should be 45.7529 m (with a few millimeters
uncertainty, perhaps). So the difference is 0.8272 m. On the
other hand, if I move the position half a pixel = 1.25 arc
minutes east and south, that is
145d1.25'E 12d58.75'N
then Charles's calculator gives me 44.9287 m, so the difference
is now just 3 mm from the gtx result for the original position.
More evidence: gdalinfo on Charles's file egm2008-2_5.pgm
(from http://geographiclib.sourceforge.net/html/geoid.html) says
Origin = (-0.020833333333333,90.020833333333329)
Pixel Size = (0.041666666666667,-0.041666666666667)
so its origin is, indeed, half a pixel farther east and south
(well, there is a also 180 degree longitude difference due to
the longitude range being 0 to 360 in this file).
I guess I could file a ticket, but I am not quite convinced
that I am right. Has anyone else noticed any problems with
the gtx file?
Another issue with the gtx file: I would have preferred if it had
one more column; that is, if the column for 180dW was repeated
for 180dE. That would make it simpler to interpolate results for
a position slightly west of 180dE.
Regards,
Mikael Rittri
Carmenta
Sweden
http://www.carmenta.com
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