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MAGNETICFIELD(1)	    GeographicLib Utilities	      MAGNETICFIELD(1)

NAME
       MagneticField -- compute the earth's magnetic field

SYNOPSIS
       MagneticField [ -n name ] [ -d dir ] [ -t time | -c time lat h ] [ -r ]
       [ -w ] [ -T tguard ] [ -H hguard ] [ -p prec ] [ -v ] [
       --comment-delimiter commentdelim ] [ --version | -h | --help ] [
       --input-file infile | --input-string instring ] [ --line-separator
       linesep ] [ --output-file outfile ]

DESCRIPTION
       MagneticField reads in times and positions on standard input and prints
       out the geomagnetic field on standard output and, optionally, its rate
       of change.

       The input line is of the form time lat lon h. time is a date of the
       form 2012-07-03, a fractional year such as 2012.5, or the string "now".
       lat and lon are the latitude and longitude expressed as decimal degrees
       or degrees, minutes, and seconds; for details on the allowed formats
       for latitude and longitude, see the "GEOGRAPHIC COORDINATES" section of
       GeoConvert(1).  h is the height above the ellipsoid in meters; this is
       optional and defaults to zero.  Alternatively, time can be given on the
       command line as the argument to the -t option, in which case it should
       not be included on the input lines.  Finally, the magnetic field can be
       computed at various points on a circle of latitude (constant time, lat,
       and h) via the -c option; in this case only the longitude should be
       given on the input lines.

       The output consists of the following 7 items:

	 the declination (the direction of the horizontal component of
	   the magnetic field measured clockwise from north) in degrees,
	 the inclination (the direction of the magnetic field measured
	   down from the horizontal) in degrees,
	 the horizontal field in nanotesla (nT),
	 the north component of the field in nT,
	 the east component of the field in nT,
	 the vertical component of the field in nT (down is positive),
	 the total field in nT.

       If the -r option is given, a second line is printed giving the rates of
       change of these quantities in degrees/yr and nT/yr.

       The WGS84 ellipsoid is used, a = 6378137 m, f = 1/298.257223563.

OPTIONS
       -n  use magnetic field model name instead of the default "wmm2015".
	   See "MODELS".

       -d  read magnetic models from dir instead of the default.  See
	   "MODELS".

       -t  evaluate the field at time instead of reading the time from the
	   input lines.

       -c  evaluate the field on a circle of latitude given by time, lat, h
	   instead of reading these quantities from the input lines.  In this
	   case, MagneticField can calculate the field considerably more
	   quickly.

       -r  toggle whether to report the rates of change of the field.

       -w  on input and output, longitude precedes latitude (except that on
	   input this can be overridden by a hemisphere designator, N, S, E,
	   W).

       -T  signal an error if time lies tguard years (default 50 yr) beyond
	   the range for the model.

       -H  signal an error if h lies hguard meters (default 500000 m) beyond
	   the range for the model.

       -p  set the output precision to prec (default 1).  Fields are printed
	   with precision with prec decimal places; angles use prec + 1
	   places.

       -v  print information about the magnetic model on standard error before
	   processing the input.

       --comment-delimiter
	   set the comment delimiter to commentdelim (e.g., "#" or "//").  If
	   set, the input lines will be scanned for this delimiter and, if
	   found, the delimiter and the rest of the line will be removed prior
	   to processing and subsequently appended to the output line
	   (separated by a space).

       --version
	   print version and exit.

       -h  print usage, the default magnetic path and name, and exit.

       --help
	   print full documentation and exit.

       --input-file
	   read input from the file infile instead of from standard input; a
	   file name of "-" stands for standard input.

       --input-string
	   read input from the string instring instead of from standard input.
	   All occurrences of the line separator character (default is a
	   semicolon) in instring are converted to newlines before the reading
	   begins.

       --line-separator
	   set the line separator character to linesep.	 By default this is a
	   semicolon.

       --output-file
	   write output to the file outfile instead of to standard output; a
	   file name of "-" stands for standard output.

MODELS
       MagneticField computes the geomagnetic field using one of the following
       models

	   wmm2010, the World Magnetic Model 2010, which approximates the
	     main magnetic field for the period 2010-2015.  See
	     http://ngdc.noaa.gov/geomag/WMM/DoDWMM.shtml
	   wmm2015, the World Magnetic Model 2015, which approximates the
	     main magnetic field for the period 2015-2020.  See
	     http://ngdc.noaa.gov/geomag/WMM/DoDWMM.shtml
	   igrf11, the International Geomagnetic Reference Field (11th
	     generation), which approximates the main magnetic field for
	     the period 1900-2015.  See
	     http://ngdc.noaa.gov/IAGA/vmod/igrf.html
	   igrf12, the International Geomagnetic Reference Field (12th
	     generation), which approximates the main magnetic field for
	     the period 1900-2020.  See
	     http://ngdc.noaa.gov/IAGA/vmod/igrf.html
	   emm2010, the Enhanced Magnetic Model 2010, which approximates
	     the main and crustal magnetic fields for the period 2010-2015.
	     See http://ngdc.noaa.gov/geomag/EMM/index.html
	   emm2015, the Enhanced Magnetic Model 2015, which approximates
	     the main and crustal magnetic fields for the period 2000-2020.
	     See http://ngdc.noaa.gov/geomag/EMM/index.html

       These models approximate the magnetic field due to the earth's core and
       (in the case of emm2010) its crust.  They neglect magnetic fields due
       to the ionosphere, the magnetosphere, nearby magnetized materials,
       electrical machinery, etc.

       By default, the "wmm2015" magnetic model is used.  This may changed by
       setting the environment variable "GEOGRAPHICLIB_MAGNETIC_NAME" or with
       the -n option.

       The magnetic models will be loaded from a directory specified at
       compile time.  This may changed by setting the environment variables
       "GEOGRAPHICLIB_MAGNETIC_PATH" or "GEOGRAPHICLIB_DATA", or with the -d
       option.	The -h option prints the default magnetic path and name.  Use
       the -v option to ascertain the full path name of the data file.

       Instructions for downloading and installing magnetic models are
       available at
       <http://geographiclib.sf.net/html/magnetic.html#magneticinst>.

ENVIRONMENT
       GEOGRAPHICLIB_MAGNETIC_NAME
	   Override the compile-time default magnetic name of "wmm2015".  The
	   -h option reports the value of GEOGRAPHICLIB_MAGNETIC_NAME, if
	   defined, otherwise it reports the compile-time value.  If the -n
	   name option is used, then name takes precedence.

       GEOGRAPHICLIB_MAGNETIC_PATH
	   Override the compile-time default magnetic path.  This is typically
	   "/usr/local/share/GeographicLib/magnetic" on Unix-like systems and
	   "C:/ProgramData/GeographicLib/magnetic" on Windows systems.	The -h
	   option reports the value of GEOGRAPHICLIB_MAGNETIC_PATH, if
	   defined, otherwise it reports the compile-time value.  If the -d
	   dir option is used, then dir takes precedence.

       GEOGRAPHICLIB_DATA
	   Another way of overriding the compile-time default magnetic path.
	   If it is set (and if GEOGRAPHICLIB_MAGNETIC_PATH is not set), then
	   $GEOGRAPHICLIB_DATA/magnetic is used.

ERRORS
       An illegal line of input will print an error message to standard output
       beginning with "ERROR:" and causes MagneticField to return an exit code
       of 1.  However, an error does not cause MagneticField to terminate;
       following lines will be converted.  If time or h are outside the
       recommended ranges for the model (but inside the ranges increase by
       tguard and hguard), a warning is printed on standard error and the
       field (which may be inaccurate) is returned in the normal way.

EXAMPLES
       The magnetic field from WMM2015 in Timbuktu on 2016-01-01

	   echo 2016-01-01 16:46:33N 3:00:34W 300 | MagneticField -r
	   => -2.12 12.15 33871.9 33848.7 -1251.4 7293.9 34648.3
	      0.09 -0.08 31.8 33.8 53.7 -41.4 22.3

       The first two numbers returned are the declination and inclination of
       the field.  The second line gives the annual change.

SEE ALSO
       GeoConvert(1), geographiclib-get-magnetic(8).

AUTHOR
       MagneticField was written by Charles Karney.

HISTORY
       MagneticField was added to GeographicLib,
       <http://geographiclib.sf.net>, in version 1.15.

GeographicLib 1.45		  2015-09-30		      MAGNETICFIELD(1)
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