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NAME

       utm2ll  -  Convert  UTM  coordinates to latitude/longitude geographical
       coordinates

SYNOPSIS

       utm2ll [-L] | [utm_x utm_y zone [nad27 | nad83 | wgs84]]

DESCRIPTION

       This program uses  Redfearn’s  formulas  to  convert  a  given  set  of
       Universal  Transverse  Mercator  (UTM)  coordinates into the equivalent
       latitude and longitude geographical coordinates.   (This  operation  is
       often   referred   to  as  inverse  projection,  since  it  projects  a
       previously-projected flat surface back onto  the  curved  surface  from
       whence  it originally came.)  The inputs are the UTM "x" (also known as
       easting) value, the UTM "y" (also known as northing) value, and the utm
       zone.   The  "x"  value includes the normal 500,000 false easting.  The
       "y" value includes the normal 10,000,000 false northing, if  the  point
       is  in the southern hemisphere.  For points in the southern hemisphere,
       make the zone number negative.

       Warning:  Not all of the possible triples of  utm_x,  utm_y,  and  zone
       values  represent  correct UTM coordinates.  The program will generally
       still  produce  latitude/longitude  coordinates,  even  for   incorrect
       inputs.   You can check that your original inputs were correct by using
       ll2utm to convert the  latitude/longitude  coordinates  back  into  UTM
       coordinates.

       The output takes the form of a single line, containing the latitude and
       longitude, separated  by  white  space.   The  values  are  in  decimal
       degrees;  with  latitudes  south  of  the  equator  being negative, and
       longitudes west of the prime meridian being negative.

       If you provide just the  "-L"  option,  the  program  will  print  some
       license information and exit.

       Projections,  and  inverse projections, depend on defining an ellipsoid
       that approximates the shape of the earth (the reference ellipsoid)  and
       defining  reference  coordinates (the datum) that allow measurements to
       be made.  Different choices  of  the  ellipsoid  and  datum  can  yield
       projections that differ by tens of meters.  There are a wide variety of
       choices,  due  to  both  the  historical  progression  of   measurement
       technology,  and  the  desire  to maximize accuracy over a given region
       (such as North America, or one of the United States).

       This program defaults to the North American Datum of 1927 (NAD-27) with
       the  Clarke Ellipsoid of 1866, since these appear to be appropriate for
       much of the freely-available data.  The  data  are  apparently  in  the
       process  of  being  converted  to  the  Geodetic  Reference System 1980
       (GRS-80) ellipsoid and NAD-83.  If you come across such data,  you  can
       specify  "nad83"  on  the command line.  The GTOPO30 data use the World
       Geodetic System 1984  (WGS-84)  ellipsoid,  which  can  be  invoked  by
       specifying "wgs84" on the command line.

SEE ALSO

       The ll2utm(1) command provides the inverse conversion.

                                 Jul 24, 2001