HELP!! Clark66->WGS84 ???#%@*!
Michael Shapiro
shapiro at zorro.cecer.army.mil
Wed Aug 26 09:59:04 EDT 1992
It isn't quite so simple. UTM is a projection and is valid for
any spheroid. Many of the older and recent map data is based on
the North American Datum of 1927 (NAD27) which uses the clark66
spheroid. This is for the latitude and longitude coordinates,
which are then projected to UTM (or Albers or Lamberts or
some other projection).
The switch to NAD83 isn't as simple as converting UTM coordinates
back to lat-long using the clark66 spheroid, then from lat-long
to UTM using WGS84.
The "datum" not only specifies the spheroid, but the orientation
of the spheroid with respect to the earth itself. The NAD27 is
not an earth centered datum while NAD83 is (i.e., for NAD27 the
center of the clark66 spheroid isn't at the center of the earth,
while the center of the WGS84 spheroid is at earth center). This
means that the lat-long coordinates change when you go from
NAD27 to NAD83. There is no program in GRASS to perform
this part of the transformation.
Recent quad sheets have approximate datum shifts for the corners
of the map and perhaps can be used to devise a linear shift for
the entire map.
|
|Date sent: 25-AUG-1992 21:39:15
|Thanks Fred:
|
|But this brings up the question what spheriod are the UTM data referenced
|too?? or isn't it referenced to a spheroid at all ?! (I'll look into it).
|
|>If I understand your question it is quite easy to get the results you want
|>the site data from the clark66 data set should be routed through m.ll2u
|>with the spheroid set to clark66 while the WGS84 stuff would be routed through
|>with the spheroid set to wgs84. Both will come out in the correct UTM zone
|>with the differences in the spheroids corrected.
|
|Thanks again,
|
|Gerry Hatcher
|
|Ocean Mapping Development Center| gerry at omdc.gso.uri.edu {Internet}
|University of Rhode Island | cbeam::gerry {span}
|voice (401)-792-6940 | fax (401)-792-6849
|
|
|
Michael
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