NAME¶
Geo::Coordinates::OSGB - Convert coordinates between Lat/Lon and the British
National Grid
An implementation of co-ordinate conversion for England, Wales, and Scotland
based on formulae published by the Ordnance Survey of Great Britain.
These modules will convert accurately between an OSGB national grid reference
and lat/lon coordinates based on the OSGB geoid model. (For an explanation of
what a geoid model is and why you should care, read the Theory section below.)
The OSGB geoid model fits mainland Britain very well, but is rather different
from the international WGS84 model that has rapidly become the de facto
universal standard model thanks to the popularity of GPS devices and maps on
the Internet. So, if you are trying to translate from an OSGB grid reference
to lat/lon coordinates that can be used in Google Earth, Wikipedia, or some
other Internet based tool, you will need to do two transformations: first
translate your grid ref into OSGB lat/lon; then nudge the result into WGS84.
Routines are provided to do both of these operations, but they are only
approximate. The inaccuracy of the approximation varies according to where you
are in the country but may be as much as several metres in some areas.
To get more accurate results you need to combine this module with its companion
Geo::Coordinates::OSTN02 which implements the transformation that now defines
the relationship between GPS survey data based on WGS84 and the British
National Grid. Using this module you should be able to get results that are
accurate to within a few centimetres, but it is slightly slower and requires
more memory to run.
Note that the OSGB (and therefore this module) does not cover the whole of the
British Isles, nor even the whole of the UK, in particular it covers neither
the Channel Islands nor Northern Ireland. The coverage that is included is
essentially the same as the coverage provided by the OSGB
"Landranger" 1:50000 series maps.
VERSION¶
Examine $Geo::Coordinates::OSGB::VERSION for details.
SYNOPSIS¶
use Geo::Coordinates::OSGB qw(ll_to_grid grid_to_ll);
# Basic conversion routines
($easting,$northing) = ll_to_grid($lat,$lon);
($lat,$lon) = grid_to_ll($easting,$northing);
DESCRIPTION¶
These modules provide a collection of routines to convert between coordinates
expressed as latitude & longtitude and map grid references, using the
formulae given in the British Ordnance Survey's excellent information leaflet,
referenced below in the Theory section. There are some key concepts explained
in that section that you need to know in order to use these modules
successfully, so you are recommended to at least skim through it now.
The module is implemented purely in Perl, and should run on any Perl platform.
In this description `OS' means `the Ordnance Survey of Great Britain': the
British government agency that produces the standard maps of England, Wales,
and Scotland. Any mention of `sheets' or `maps' refers to one or more of the
204 sheets in the 1:50,000 scale `Landranger' series of OS maps.
This code is fine tuned to the British national grid system. You could use it
elsewhere but you would need to adapt it. Some starting points for doing this
are explained in the Theory section below.
SUBROUTINES/METHODS¶
The following functions can be exported from the
"Geo::Coordinates::OSGB" module:
grid_to_ll ll_to_grid
shift_ll_into_WGS84 shift_ll_from_WGS84
parse_grid
parse_trad_grid format_grid_trad
parse_GPS_grid format_grid_GPS
parse_landranger_grid format_grid_landranger
parse_ISO_ll format_ll_trad
format_ll_ISO
None of these is exported by default, so pick the ones you want or use an
":all" tag to import them all at once.
use Geo::Coordinates::OSGB ':all';
- ll_to_grid(lat,lon)
- When called in a void context, or with no arguments "ll_to_grid"
does nothing.
When called in a list context, "ll_to_grid" returns two numbers
that represent the easting and the northing corresponding to the latitude
and longitude supplied.
The parameters can be supplied as real numbers representing decimal degrees,
like this
my ($e,$n) = ll_to_grid(51.5, 2.1);
Following the normal convention, positive numbers mean North or East,
negative South or West. If you have data with degrees, minutes and
seconds, you can convert them to decimals like this:
my ($e,$n) = ll_to_grid(51+25/60, 0-5/60-2/3600);
Or you can use a single string in ISO 6709 form, like this:
my ($e,$n) = ll_to_grid('+5130-00005/');
To learn exactly what is matched by this last option, read the source of the
module and look for the definition of $ISO_LL_PATTERN. Note that the
neither the "+" or "-" signs at the beginning and in
the middle, nor the trailing "/" may be omitted.
If you have trouble remembering the order of the arguments, or the returned
values, note that latitude comes before longitude in the alphabet too, as
easting comes before northing.
The easting and northing will be returned as a whole number of metres from
the point of origin of the British Grid (which is a point a little way to
the south-west of the Scilly Isles).
If you want the result presented in a more traditional grid reference format
you should pass the results to one of the grid formatting routines, which
are described below. Like this.
$gridref = format_grid_trad(ll_to_grid(51.5,-0.0833));
$gridref = format_grid_GPS(ll_to_grid(51.5,-0.0833));
$gridref = format_grid_landranger(ll_to_grid(51.5,-0.0833));
However if you call "ll_to_grid" in a scalar context, it will
automatically call "format_grid_trad" for you.
It is not needed for any normal work, but "ll_to_grid()" also
takes an optional argument that sets the ellipsoid model to use. This
normally defaults to `OSGB36', the name of the normal model for working
with British maps. If you are working with the highly accurate OSTN02
conversions supplied in the companion module in this distribution, then
you will need to produce pseudo-grid references as input to those
routines. For these purposes you should call "ll_to_grid()" like
this:
my $pseudo_gridref = ll_to_grid(51.2, -0.4, 'WGS84');
and then transform this to a real grid reference using
"ETRS89_to_OSGB36()" from the companion module. This is
explained in more detail below.
- format_grid_trad(e,n)
- Formats an (easting, northing) pair into traditional `full national grid
reference' with two letters and two sets of three numbers, like this `TQ
102 606'. If you want to remove the spaces, just apply "s/\s//g"
to it.
$gridref = format_grid_trad(533000, 180000); # TQ 330 800
$gridref =~ s/\s//g; # TQ330800
If you want the individual components call it in a list context.
($sq, $e, $n) = format_grid_trad(533000, 180000); # (TQ,330,800)
Note the easting and northing are truncated to hectometers (as the OS system
demands), so the grid reference refers to the lower left corner of the
relevant 100m square.
- format_grid_GPS(e,n)
- Users who have bought a GPS receiver may initially have been puzzled by
the unfamiliar format used to present coordinates in the British national
grid format. On my Garmin Legend C it shows this sort of thing in the
display.
TQ 23918
bng 00972
and in the track logs the references look like this "TQ 23918
00972".
These are just the same as the references described on the OS sheets, except
that the units are metres rather than hectometres, so you get five digits
in each of the easting and northings instead of three. So in a scalar
context "format_grid_GPS()" returns a string like this:
$gridref = format_grid_GPS(533000, 180000); # TQ 33000 80000
If you call it in a list context, you will get a list of square, easting,
and northing, with the easting and northing as metres within the grid
square.
($sq, $e, $n) = format_grid_GPS(533000, 180000); # (TQ,33000,80000)
Note that, at least until WAAS is working in Europe, the results from your
GPS are unlikely to be more accurate than plus or minus 5m even with
perfect reception. Most GPS devices can display the accuracy of the
current fix you are getting, but you should be aware that all normal
consumer-level GPS devices can only ever produce an approximation of an OS
grid reference, no matter what level of accuracy they may display. The
reasons for this are discussed below in the section on Theory.
- format_grid_landranger(e,n)
- This routine does the same as "format_grid_trad", but it appends
the number of the relevant OS Landranger 1:50,000 scale map to the
traditional grid reference. Note that there may be several or no sheets
returned. This is because many (most) of the Landranger sheets overlap,
and many other valid grid references are not on any of the sheets (because
they are in the sea or a remote island. This module does not yet cope with
the detached insets on some sheets.
In a list context you will get back a list like this: (square, easting,
northing, sheet) or (square, easting, northing, sheet1, sheet2) etc. There
are a few places where three sheets overlap, and one corner of
Herefordshire which appears on four maps (sheets 137, 138, 148, and 149).
If the GR is not on any sheet, then the list of sheets will be empty.
In a scalar context you will get back the same information in a helpful
string form like this "NN 241 738 on OS Sheet 44". Note that the
easting and northing will have been truncated to the normal hectometre
three digit form. The idea is that you'll use this form for people who
might actually want to look up the grid reference on the given map sheet,
and the traditional GR form is quite enough accuracy for that
purpose.
- parse_trad_grid(grid_ref)
- Turns a traditional grid reference into a full easting and northing pair
in metres from the point of origin. The grid_ref can be a string
like 'TQ203604' or 'SW 452 004', or a list like this "('TV',
'435904')" or a list like this "('NN', '345', '208')".
- parse_GPS_grid(grid_ref)
- Does the same as "parse_trad_grid" but is looking for five digit
numbers like 'SW 45202 00421', or a list like this "('NN', '34592',
'20804')".
- parse_landranger_grid(sheet, e, n)
- This converts an OS Landranger sheet number and a local grid reference
into a full easting and northing pair in metres from the point of origin.
The OS Landranger sheet number should be between 1 and 204 inclusive (but I
may extend this when I support insets). You can supply "(e,n)"
as 3-digit hectometre numbers or 5-digit metre numbers. In either case if
you supply any leading zeros you should 'quote' the numbers to stop Perl
thinking that they are octal constants.
This module will croak at you if you give it an undefined sheet number, or
if the grid reference that you supply does not exist on the sheet.
In order to get just the coordinates of the SW corner of the sheet, just
call it with the sheet number. It is easy to work out the coordinates of
the other corners, because all OS Landranger maps cover a 40km square (if
you don't count insets or the occasional sheet that includes extra details
outside the formal margin).
- parse_grid(grid_ref)
- Attempts to match a grid reference some form or other in the input string
and will then call the appropriate grid parsing routine from those defined
above. In particular it will parse strings in the form '176-345210'
meaning grid ref 345 210 on sheet 176, as well as 'TQ345210' and 'TQ 34500
21000' etc. You can in fact always use "parse_grid" instead of
the more specific routines unless you need to be picky about the
input.
- grid_to_ll(e,n) or grid_to_ll(grid_ref)
- When called in list context "grid_to_ll()" returns a pair of
numbers representing longitude and latitude coordinates, as real numbers.
Following convention, positive numbers are North and East, negative
numbers are South and West. The fractional parts of the results represent
fractions of degrees.
When called in scalar context it returns a string in ISO longitude and
latitude form, such as '+5025-00403/' with the result rounded to the
nearest minute (the formulae are not much more accurate than this). In a
void context it does nothing.
The arguments must be an (easting, northing) pair representing the absolute
grid reference in metres from the point of origin. You can get these from
a grid reference string by calling "parse_grid()" first.
An optional last argument defines the geoid model to use just as it does for
"ll_to_grid()". This is only necessary is you are working with
the pseudo-grid references produced by the OSTN02 routines. See Theory for
more discussion.
- format_ll_trad(lat, lon)
- Takes latitude and longitude in decimal degrees as arguments and returns a
string like this
N52:12:34 W002:30:27
In a list context it returns all 8 elements (hemisphere, degrees, minutes,
seconds for each of lat and lon) in a list. In a void context it does
nothing.
- format_ll_ISO(lat, lon)
- Takes latitude and longitude in decimal degrees as arguments and returns a
string like this
+5212-00230/
In a list context it returns all 6 elements (sign, degrees, minutes for each
of lat and lon) in a list. In a void context it does nothing.
- parse_ISO_ll(ISO_string)
- Reads an ISO 6709 formatted location identifier string such as
'+5212-00230/'. To learn exactly what is matched by this last option, read
the source of the module and look for the definition of $ISO_LL_PATTERN.
Note that the neither the "+" or "-" signs at the
beginning and in the middle, nor the trailing "/" may be
omitted. These strings can also include the altitude of a point, in
metres, like this: '+5212-00230+140/'. If you omit the altitude, 0 is
assumed.
In a list context it returns ($lat, $lon, $altitude). So if you don't want
or don't need the altitude, you should just drop it, for example like
this:
my ($lat, $lon) = parse_ISO_ll('+5212-00230/')
In normal use you won't notice this. In particular you don't need to worry
about it when passing the results on to "ll_to_grid", as that
routine looks for an optional altitude after the lat/lon.
- shift_ll_from_WGS84(lat, lon, altitude)
- Takes latitude and longitude in decimal degrees (plus an optional altitude
in metres) from a WGS84 source (such as your GPS handset or Google Earth)
and returns an approximate equivalent latitude and longitude according to
the OSGM02 model. To determine the OSGB grid reference for given WGS84
lat/lon coordinates, you should call this before you call
"ll_to_grid". Like so:
($lat, $lon, $alt) = shift_ll_from_WGS84($lat, $lon, $alt);
($e, $n) = ll_to_grid($lat,$lon);
You don't need to call this to determine a grid reference from lat/lon
coordinates printed on OSGB maps (the so called "graticule
intersections" marked in pale blue on the Landranger series).
This routine provide a fast approximation; for a slower, more accurate
approximation use the companion Geo::Coordinates::OSTN02 modules.
- shift_ll_into_WGS84(lat, lon, altitude)
- Takes latitude and longitude in decimal degrees (plus an optional altitude
in metres) from an OSGB source (such as coordinates you read from a
Landranger map, or more likely coordinates returned from
"grid_to_ll()") and adjusts them to fit the WGS84 model.
To determine WGS84 lat/lon coordinates (for use in Wikipedia, or Google
Earth etc) for a given OSGB grid reference, you should call this after you
call "grid_to_ll()". Like so:
($lat, $lon) = grid_to_ll($e, $n);
($lat, $lon, $alt) = shift_ll_into_WGS84($lat, $lon, $alt);
This routine provide a fast approximation; for a slower, more accurate
approximation use the companion Geo::Coordinates::OSTN02 modules.
THEORY¶
The algorithms and theory for these conversion routines are all from
A Guide
to Coordinate Systems in Great Britain published by the OSGB, April 1999
(Revised Dec 2010) and available at
http://www.ordnancesurvey.co.uk/.
You may also like to read some of the other introductory material there. Should
you be hoping to adapt this code to your own custom Mercator projection, you
will find the paper called
Surveying with the National GPS
Network, especially useful.
The routines are intended for use in Britain with the Ordnance Survey's National
Grid, however they are written in an entirely generic way, so that you could
adapt them to any other ellipsoid model that is suitable for your local area
of the earth. There are other modules that already do this that may be more
suitable (which are referenced in the "See Also" section), but the
key parameters are all defined at the top of the module.
$ellipsoid_shapes{OSGB36} = [ 6377563.396, 6356256.910 ];
use constant ORIGIN_LONGITUDE => RAD * -2; # lon of grid origin
use constant ORIGIN_LATITUDE => RAD * 49; # lat of grid origin
use constant ORIGIN_EASTING => 400000; # Easting for origin
use constant ORIGIN_NORTHING => -100000; # Northing for origin
use constant CONVERGENCE_FACTOR => 0.9996012717; # Convergence factor
The ellipsoid model is defined by two numbers that represent the major and minor
radius measured in metres. The Mercator grid projection is then defined by the
other five parameters. The general idea is that you pick a suitable point to
start the grid that minimizes the inevitable distortion that is involved in a
Mercator projection from spherical to Euclidean coordinates. Such a point
should be on a meridian that bisects the area of interest and is nearer to the
equator than the whole area. So for Britain the point of origin is 2W and 49N
(in the OSGB geoid model) which is near the Channel Islands. This point should
be set as the "ORIGIN_LONGITUDE" and "ORIGIN_LATITUDE"
parameters (as above) measured in radians. Having this True Point of Origin in
the middle and below (or above if you are antipodean) minimizes distortion but
means that some of the grid values would be negative unless you then also
adjust the grid to make sure you do not get any negative values in normal use.
This is done by defining the grid coordinates of the True Point of Origin to
be such that all the coordinates in the area of interest will be positive.
These are the parameters "ORIGIN_EASTING" and
"ORIGIN_NORTHING". For Britain the coordinates are set as 400000 and
-100000, so the that point (0,0) in the grid is just to the south west of the
Scilly Isles. This (0,0) point is called the False Point of Origin. The fifth
parameter affects the convergence of the Mercator projection as you get nearer
the pole; this is another feature designed to minimize distortion, and if in
doubt set it to 1 (which means it has no effect). For Britain, being so
northerly it is set to slightly less than 1.
The British National Grid¶
One consequence of the True Point of Origin of the British Grid being set to
"+4900-00200/" is that all the vertical grid lines are parallel to
the 2W meridian; you can see this on the appropriate OS maps (for example
Landranger sheet 184), or on the "plotmaps.pdf" picture supplied
with this package. The effect of moving the False Point of Origin to the far
south west is that all grid references always positive.
Strictly grid references are given as whole numbers of metres from this point,
with the easting always given before the northing. For everyday use however,
the OSGB suggest that grid references need only to be given within the local
100km square as this makes the numbers smaller. For this purpose they divide
Britain into a series of 100km squares identified in pair of letters: TQ, SU,
ND, etc. The grid of the big squares actually used is something like this:
HP
HU
HY
NA NB NC ND
NF NG NH NJ NK
NL NM NN NO NP
NR NS NT NU
NW NX NY NZ
SC SD SE TA
SH SJ SK TF TG
SM SN SO SP TL TM
SR SS ST SU TQ TR
SV SW SX SY SZ TV
SW covers most of Cornwall, TQ London, and HU the Shetlands. Note that it has
the neat feature that N and S are directly above each other, so that most Sx
squares are in the south and most Nx squares are in the north.
Within each of these large squares, we only need five digit coordinates --- from
(0,0) to (99999,99999) --- to refer to a given square metre. For daily use
however we don't generally need such precision, so the normal recommended
usage is to use units of 100m (hectometres) so that we only need three digits
for each easting and northing --- 000,000 to 999,999. If we combine the
easting and northing we get the familiar traditional six figure grid
reference. Each of these grid references is repeated in each of the large
100km squares but for local use with a particular map, this does not usually
matter. Where it does matter, the OS suggest that the six figure reference is
prefixed with the identifier of the large grid square to give a `full national
grid reference', such as TQ330800. This system is described in the notes of in
the corner of every Landranger 1:50,000 scale map.
Modern GPS receivers can all display coordinates in the OS grid system. You just
need to set the display units to be `British National Grid' or whatever
similar name is used on your unit. Most units display the coordinates as two
groups of five digits and a grid square identifier. The units are metres
within the grid square (although beware that the GPS fix is unlikely to be
accurate down to the last metre).
Geoid models¶
This section explains the fundamental problems of mapping a spherical earth onto
a flat piece of paper (or computer screen). A basic understanding of this
material will help you use these routines more effectively. It will also
provide you with a good store of ammunition if you ever get into an argument
with someone from the Flat Earth Society.
It is a direct consequence of Newton's law of universal gravitation (and in
particular the bit that states that the gravitational attraction between two
objects varies inversely as the square of the distance between them) that all
planets are roughly spherical. (If they were any other shape gravity would
tend to pull them into a sphere). On the other hand, most useful surfaces for
displaying large scale maps (such as pieces of paper or screens) are flat.
There is therefore a fundamental problem in making any maps of the earth that
its curved surface being mapped must be distorted at least slightly in order
to get it to fit onto the flat map.
This module sets out to solve the corresponding problem of converting latitude
and longitude coordinates (designed for a spherical surface) to and from a
rectangular grid (for a flat surface). This projection is in itself is a
fairly lengthy bit of maths, but what makes it extra complicated is that the
earth is not quite a sphere. Because our planet spins about a vertical axis,
it tends to bulge out slightly in the middle, so it is more of an oblate
spheroid than a sphere. This makes the maths even longer, but the real problem
is that the earth is not a regular oblate spheroid either, but an irregular
lump that closely resembles an oblate spheroid and which is constantly (if
slowly) being rearranged by plate tectonics. So the best we can do is to pick
an imaginary regular oblate spheroid that provides a good fit for the region
of the earth that we are interested in mapping. The British Ordnance Survey
did this back in 1830 and have used it ever since as the base on which the
National Grid for Great Britain is constructed. You can also call an oblate
spheroid an ellipsoid if you like. The general term for an ellipsoid model of
the earth is a "geoid".
The first standard OSGB geoid is known as "Airy 1830" after the year
of its first development. It was revised in 1936, and that version, generally
known as OSGB36, is the basis of all current OSGB mapping. In 2002 the model
was redefined (but not functionally changed) as a transformation from the
international geoid model WGS84. This redefinition is called OSGM02. For the
purposes of these modules (and most other purposes) OSGB36 and OSGM02 may be
treated as synonyms.
The general idea is that you can establish your latitude and longitude by
careful observation of the sun, the moon, the planets, or your GPS handset,
and that you then do some clever maths to work out the corresponding grid
reference using a suitable geoid. These modules let you do the clever maths,
and the geoid they use is the OSGM02 one. This model provides a good match to
the local shape of the Earth in the British Isles, but is not designed for use
in the rest of the world; there are many other models in use in other
countries.
In the mid-1980s a new standard geoid model was defined to use with the
fledgling global positioning system (GPS). This model is known as WGS84, and
is designed to be a compromise model that works equally well for all parts of
the globe (or equally poorly depending on your point of view --- for one thing
WGS84 defines the Greenwich observatory in London to be not quite on the zero
meridian). Nevertheless WGS84 has grown in importance as GPS systems have
become consumer items and useful global mapping tools (such as Google Earth)
have become freely available through the Internet. Most latitude and longitude
coordinates quoted on the Internet (for example in Wikipedia) are WGS84
coordinates.
One thing that should be clear from the theory is that there is no such thing as
a single definitive set of coordinates for every unique spot on earth. There
are only approximations based on one or other of the accepted geoid models,
however for most practical purposes good approximations are all you need. In
Europe the official definition of WGS84 is sometime referred to as ETRS89. For
all practical purposes in Western Europe the OS advise that one can regard
ETRS89 as identical to WGS84 (unless you need to worry about tectonic plate
movements).
Practical implications¶
If you are working exclusively with British OS maps and you merely want to
convert from the grid to the latitude and longitude coordinates printed (as
faint blue crosses) on those maps, then all you need from these modules are
the plain "grid_to_ll()" and "ll_to_grid()" routines. On
the other hand if you want to produce latitude and longitude coordinates
suitable for Google Earth or Wikipedia from a British grid reference, then you
need an extra step. Convert your grid reference using "grid_to_ll()"
and then shift it from the OSGB model to the WGS84 model using
"shift_ll_into_WGS84()". To go the other way round, shift your WGS84
lat/lon coordinated into OSGB, using "shift_ll_from_WGS84()", before
you convert them using "ll_to_grid()".
If you have a requirement for really accurate work (say to within a millimetre
or two) then you need to use the OS's transformation matrix called OSTN02.
This monumental work published in 2002 re-defined the British grid in terms of
offsets from WGS84 to allow really accurate grid references to be determined
from really accurate GPS readings (the sort you get from professional fixed
base stations, not from your car's sat nav or your hand-held device). The
problem with it is that it defines the grid in terms of a deviation in three
dimensions from a pseudo-grid based on WGS84 and it does this separately for
every square km of the country, so the data set is huge and takes a second or
two to load even on a fast machine. Nevertheless a Perl version of OSTN02 is
included as a separate module in this distribution just in case you really
need it (but you don't need it for any "normal" work). Because of
the way OSTN02 is defined, the sequence of conversion and shifting works
differently from the approximate routines described above.
Starting with a really accurate lat/lon reading in WGS84 terms, you need to
transform it into a pseudo-grid reference using "ll_to_grid()" using
an optional argument to tell it to use the WGS84 geoid parameters instead of
the default OSGB parameters. The Geo::Coordinates::OSTN02 package provides a
routine called "ETRS89_to_OSGB36()" which will shift this
pseudo-grid reference into an accurate OSGB grid reference. To go back the
other way, you use "OSGB36_to_ETRS89()" to make a pseudo-grid
reference, and then call "grid_to_ll()" with the WGS84 parameter to
get WGS84 lat/long coordinates.
($lat, $lon, $height) = (51.5, -1, 10);
($x, $y) = ll_to_grid($lat, $lon, 'WGS84');
($e, $n, $elevation) = ETRS89_to_OSGB36($x, $y, $height);
($x, $y, $z) = OSGB36_to_ETRS89($e, $n, $elevation);
($lat, $lon) = grid_to_ll($x, $y, 'WGS84');
EXAMPLES¶
# to import everything try...
use Geo::Coordinates::OSGB ':all';
# Get full coordinates in metres from GR
($e,$n) = parse_trad_grid('TQ 234 098');
# Latitude and longitude according to the OSGB geoid (as
# printed on OS maps), if you want them to work in Google
# Earth or some other tool that uses WGS84 then adjust results
($lat, $lon) = grid_to_ll($e, $n);
($lat, $lon, $alt) = shift_ll_into_WGS84($lat, $lon, $alt);
# and to go the other way
($lat, $lon, $alt) = shift_ll_from_WGS84($lat, $lon, $alt);
($e, $n) = ll_to_grid($lat,$lon);
# In both cases the elevation is in metres (default=0m)
# Reading and writing grid references
# Format full easting and northing into traditional formats
$gr1 = format_grid_trad($e, $n); # "TQ 234 098"
$gr1 =~ s/\s//g; # "TQ234098"
$gr2 = format_grid_GPS($e, $n); # "TQ 23451 09893"
$gr3 = format_grid_landranger($e, $n);# "TQ 234 098 on Sheet 176"
# or call in list context to get the individual parts
($sq, $e, $n) = format_grid_trad($e, $n); # ('TQ', 234, 98)
# parse routines to convert from these formats to full e,n
($e,$n) = parse_grid('TQ 234 098');
($e,$n) = parse_grid('TQ234098'); # spaces optional
($e,$n) = parse_grid('TQ',234,98); # or even as a list
($e,$n) = parse_grid('TQ 23451 09893'); # as above..
# You can also get grid refs from individual maps.
# Sheet between 1..204; gre & grn must be 3 or 5 digits long
($e,$n) = parse_grid(176,123,994);
# With just the sheet number you get GR for SW corner
($e,$n) = parse_grid(184);
# Reading and writing lat/lon coordinates
($lat, $lon) = parse_ISO_ll("+52-002/");
$iso = format_ll_ISO($lat,$lon); # "+520000-0020000/"
$str = format_ll_trad($lat,$lon); # "N52:00:00 W002:00:00"
BUGS AND LIMITATIONS¶
The conversions are only approximate. So after
($a1,$b1) = grid_to_ll(ll_to_grid($a,$b));
neither "$a==$a1" nor "$b==$b1". However
"abs($a-$a1)" and "abs($b-$b1)" should be less than
0.00001 which will give you accuracy to within a metre. In the middle of the
grid 0.00001 degrees is approximately 1 metre. Note that the error increases
the further away you are from the central meridian of the grid system.
The "format_grid_landranger()" does not take account of inset areas on
the sheets. So if you feed it a reference for the Scilly Isles, it will tell
you that the reference is not on any Landranger sheet, whereas in fact the
Scilly Isles are on an inset in the SW corner of Sheet 203. There is nothing
in the design that prevents me adding the insets, they just need to be added
as extra sheets with names like "Sheet 2003 Inset 1" with their own
reference points and special sheet sizes. Collecting the data is another
matter.
Not enough testing has been done. I am always grateful for the feedback I get
from users, but especially for problem reports that help me to make this a
better module.
DIAGNOSTICS¶
Should this software not do what you expect, then please first read this
documentation, secondly verify that you have installed it correctly and that
it passes all the installation tests on your set up, thirdly study the source
code to see what it's supposed to be doing, fourthly get in touch to ask me
about it.
CONFIGURATION AND ENVIRONMENT¶
There is no configuration required either of these modules or your environment.
It should work on any recent version of perl, on any platform.
DEPENDENCIES¶
None.
INCOMPATIBILITIES¶
None known.
LICENSE AND COPYRIGHT¶
Copyright (C) 2002-2013 Toby Thurston
OSTN02 transformation data is freely available but remains Crown Copyright (C)
2002
This library is free software; you can redistribute it and/or modify it under
the same terms as Perl itself.
AUTHOR¶
Toby Thurston -- 04 Oct 2013
toby@cpan.org
SEE ALSO¶
The UK Ordnance Survey's theory paper referenced above.
See Geo::Coordinates::Convert for a general approach (not based on the above
paper).
See Geo::Coordinates::Lambert for a French approach.