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package Geo::Coordinates::OSGB; |
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8
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255305
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use base qw(Exporter); |
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65
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8
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1003
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3
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51
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use strict; |
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15
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170
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4
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37
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use warnings; |
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11
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8
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205
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5
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42
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use Carp; |
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15
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8
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519
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6
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2006
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use File::Share ':all'; |
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51205
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8
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1436
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194
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use 5.010; # at least Perl 5.10 please |
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31
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9
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our $VERSION = '2.20'; |
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11
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our %EXPORT_TAGS = ( |
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all => [ |
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qw( |
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ll_to_grid |
15
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grid_to_ll |
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17
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ll_to_grid_helmert |
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grid_to_ll_helmert |
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20
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get_ostn02_shift_pair |
21
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set_default_shape |
22
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) |
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] |
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); |
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26
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our @EXPORT_OK = ( @{ $EXPORT_TAGS{all} } ); |
27
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28
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8
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1075
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use constant ELLIPSOIDS => { |
29
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WGS84 => [ 6_378_137.000, 6_356_752.31424518, 298.257223563, 0.006694379990141316996137233540 ], |
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ETRS89 => [ 6_378_137.000, 6_356_752.314140, 298.257222101, 0.006694380022900787625359114703 ], |
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GRS80 => [ 6_378_137.000, 6_356_752.314140, 298.257222101, 0.006694380022900787625359114703 ], |
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OSGB36 => [ 6_377_563.396, 6_356_256.909, 299.3249612665, 0.0066705400741492318211148938735613129751683486352306 ], |
33
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8
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8
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56
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}; |
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18
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34
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35
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my $default_shape = 'WGS84'; |
36
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37
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sub set_default_shape { |
38
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2
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2
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1
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7
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my $s = shift; |
39
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2
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50
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9
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croak "Unknown shape: $s" if !exists ELLIPSOIDS->{$s}; |
40
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2
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7
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$default_shape = $s; |
41
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2
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5
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return; |
42
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} |
43
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44
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# constants for OSGB mercator projection |
45
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8
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8
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56
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use constant ORIGIN_LONGITUDE => -2 / 57.29577951308232087679815481410517; |
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16
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8
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480
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46
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8
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8
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57
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use constant ORIGIN_LATITUDE => 49 / 57.29577951308232087679815481410517; |
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8
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21
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8
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441
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47
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8
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8
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65
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use constant ORIGIN_EASTING => 400_000; |
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26
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8
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409
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48
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8
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8
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51
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use constant ORIGIN_NORTHING => -100_000; |
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17
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8
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389
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49
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8
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8
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46
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use constant CONVERGENCE_FACTOR => 0.9996012717; |
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8
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19
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8
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403
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50
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51
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# constants for small distances |
52
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8
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8
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49
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use constant TENTH_MM => 0.0001; |
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8
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15
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8
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356
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53
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8
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8
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44
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use constant HUNDREDTH_MM => 0.00001; |
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8
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17
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8
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544
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54
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55
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# OSTN data |
56
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my $ostn_ee_file = dist_file('Geo-Coordinates-OSGB', 'ostn_east_shift_82140'); |
57
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my $ostn_nn_file = dist_file('Geo-Coordinates-OSGB', 'ostn_north_shift_-84180'); |
58
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59
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8
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8
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46
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use constant MIN_EE_SHIFT => 82140; |
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8
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16
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8
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372
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60
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8
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8
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48
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use constant MIN_NN_SHIFT => -84180; |
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8
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22
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8
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19141
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61
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62
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sub _load_ostn_data { |
63
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16
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16
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126
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my $name = shift; |
64
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16
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1204
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open my $fh, '< :raw :bytes', $name; |
65
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16
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21612
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my $count = read $fh, my $data, 1753902; |
66
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16
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206
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close $fh; |
67
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16
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924766
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return unpack "S<[$count]", $data; # Note the byte order modifiers.... |
68
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} |
69
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70
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# Perl 5.08: I've use the byte order modifier "<" on the unpack command above |
71
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# because this means we are system independent and the binary data can be |
72
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# read of little endian and big endian machines. But this needs Perl 5.10 or |
73
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# better. If you must have perl 5.08, then you will need to get a copy of |
74
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# OSTN15 from the OSGB, modify "build/pack_ostn_data" to pack the data in your |
75
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# native format, and then modify the "unpack" above to match. |
76
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77
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my @EE_SHIFTS = _load_ostn_data($ostn_ee_file); |
78
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my @NN_SHIFTS = _load_ostn_data($ostn_nn_file); |
79
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80
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sub _llh_to_cartesian { |
81
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15
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15
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36
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my ( $lat, $lon, $H, $shape ) = @_; |
82
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83
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15
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22
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my ( $a, $b, $f, $ee ) = @{ ELLIPSOIDS->{$shape} }; |
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15
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36
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84
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85
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15
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26
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my $phi = $lat / 57.29577951308232087679815481410517; |
86
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15
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25
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my $sp = sin $phi; |
87
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15
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23
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my $cp = cos $phi; |
88
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15
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24
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my $lam = $lon / 57.29577951308232087679815481410517; |
89
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15
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22
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my $sl = sin $lam; |
90
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15
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23
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my $cl = cos $lam; |
91
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92
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15
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30
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my $nu = $a / sqrt( 1 - $ee * $sp * $sp ); |
93
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94
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15
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26
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my $x = ( $nu + $H ) * $cp * $cl; |
95
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15
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27
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my $y = ( $nu + $H ) * $cp * $sl; |
96
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15
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34
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my $z = ( ( 1 - $ee ) * $nu + $H ) * $sp; |
97
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98
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15
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34
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return ( $x, $y, $z ); |
99
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} |
100
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101
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sub _cartesian_to_llh { |
102
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15
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15
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33
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my ( $x, $y, $z, $shape ) = @_; |
103
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104
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15
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37
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my ( $a, $b, $f, $ee ) = @{ ELLIPSOIDS->{$shape} }; |
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15
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40
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105
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106
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15
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28
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my $p = sqrt($x*$x+$y*$y); |
107
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15
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61
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my $lam = atan2 $y, $x; |
108
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15
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35
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my $phi = atan2 $z, $p*(1-$ee); |
109
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110
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15
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22
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my ( $nu, $oldphi, $sp ); |
111
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15
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23
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while (1) { |
112
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45
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61
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$sp = sin $phi; |
113
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45
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63
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$nu = $a / sqrt(1 - $ee*$sp*$sp); |
114
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45
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52
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$oldphi = $phi; |
115
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45
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69
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$phi = atan2 $z+$ee*$nu*$sp, $p; |
116
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45
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100
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90
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last if abs($oldphi-$phi) < 1E-12; |
117
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} |
118
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119
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15
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23
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my $lat = $phi * 57.29577951308232087679815481410517; |
120
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15
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21
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my $lon = $lam * 57.29577951308232087679815481410517; |
121
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15
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28
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my $H = $p / cos($phi) - $nu; |
122
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123
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15
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33
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return ( $lat, $lon, $H ); |
124
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} |
125
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126
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sub _small_Helmert_transform_for_OSGB { |
127
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15
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15
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31
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my ($direction, $xa, $ya, $za) = @_; |
128
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15
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28
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my $tx = $direction * -446.448; |
129
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15
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26
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my $ty = $direction * +125.157; |
130
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15
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21
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my $tz = $direction * -542.060; |
131
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15
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23
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my $sp = $direction * 0.0000204894 + 1; |
132
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15
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24
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my $rx = ($direction * -0.1502/3600) / 57.29577951308232087679815481410517; |
133
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15
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29
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my $ry = ($direction * -0.2470/3600) / 57.29577951308232087679815481410517; |
134
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15
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25
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my $rz = ($direction * -0.8421/3600) / 57.29577951308232087679815481410517; |
135
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15
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27
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my $xb = $tx + $sp*$xa - $rz*$ya + $ry*$za; |
136
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15
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26
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my $yb = $ty + $rz*$xa + $sp*$ya - $rx*$za; |
137
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15
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34
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my $zb = $tz - $ry*$xa + $rx*$ya + $sp*$za; |
138
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15
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30
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return ($xb, $yb, $zb); |
139
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} |
140
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141
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sub _shift_ll_from_osgb36_to_wgs84 { |
142
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4
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4
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11
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my ($lat, $lon) = @_; |
143
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4
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9
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my ($xa, $ya, $za) = _llh_to_cartesian($lat, $lon, 0, 'OSGB36' ); |
144
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4
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16
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my ($xb, $yb, $zb) = _small_Helmert_transform_for_OSGB(-1,$xa, $ya, $za); |
145
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4
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11
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my ($latx, $lonx, $junk) = _cartesian_to_llh($xb, $yb, $zb, 'WGS84'); |
146
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4
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54
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return ($latx, $lonx); |
147
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} |
148
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149
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sub _shift_ll_from_wgs84_to_osgb36 { |
150
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11
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11
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21
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my ($lat, $lon) = @_; |
151
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11
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38
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my ($xa, $ya, $za) = _llh_to_cartesian($lat, $lon, 0, 'WGS84'); |
152
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11
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34
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my ($xb, $yb, $zb) = _small_Helmert_transform_for_OSGB(+1,$xa, $ya, $za); |
153
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11
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25
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my ($latx, $lonx, $junk) = _cartesian_to_llh($xb, $yb, $zb, 'OSGB36'); |
154
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11
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29
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return ($latx, $lonx); |
155
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} |
156
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157
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sub ll_to_grid { |
158
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159
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163
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163
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1
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19249
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my ( $lat, $lon, $options ) = @_; |
160
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161
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# we might have been passed a hash as the first argument |
162
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163
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50
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66
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438
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if (ref $lat && defined $lat->{lat} && defined $lat->{lon}) { |
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66
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163
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1
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3
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$options = $lat; |
164
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1
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5
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$lat = $options->{lat}; |
165
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1
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3
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$lon = $options->{lon}; |
166
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} |
167
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168
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# correct reversed arguments, this is always valid in OSGB area |
169
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163
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100
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478
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if ($lat < $lon) { |
170
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1
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3
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($lat, $lon) = ($lon, $lat) |
171
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} |
172
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173
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163
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100
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482
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my $shape = exists $options->{shape} ? $options->{shape} : $default_shape; |
174
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163
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50
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416
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croak "Unknown shape: $shape" if !exists ELLIPSOIDS->{$shape}; |
175
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176
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163
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463
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my ($e,$n) = _project_onto_grid($lat, $lon, $shape); |
177
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163
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286
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my @out; |
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# If we were using LL from OS maps, then we are done |
180
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163
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100
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351
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if ($shape eq 'OSGB36') { |
181
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12
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26
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@out = map { sprintf '%.3f', $_ } ($e, $n); |
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24
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171
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182
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12
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100
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91
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return wantarray ? @out : "@out"; |
183
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} |
184
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# now shape is WGS84 etc so we must adjust |
186
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302
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my ($dx, $dy) = _find_OSTN_shifts_at($e,$n); |
187
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100
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319
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if ($dx) { |
188
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333
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@out = map { sprintf '%.3f', $_ } ($e + $dx, $n + $dy); |
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288
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2060
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189
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144
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100
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813
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return wantarray ? @out : "@out"; |
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} |
191
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192
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# still here? Then do Helmert shift into OSGB36 and re-project |
193
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7
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51
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return ll_to_grid_helmert($lat, $lon) |
194
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} |
195
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196
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sub ll_to_grid_helmert { |
197
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11
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11
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1
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25
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my ($lat, $lon) = @_; |
198
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11
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31
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my @out = map { sprintf '%.0f', $_ } # round to metres |
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22
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71
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199
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_project_onto_grid( _shift_ll_from_wgs84_to_osgb36($lat, $lon), 'OSGB36' ); |
200
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11
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100
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86
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return wantarray ? @out : "@out"; |
201
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} |
202
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203
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sub _project_onto_grid { |
204
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205
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174
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174
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367
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my ( $lat, $lon, $shape ) = @_; |
206
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207
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174
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260
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my ($a,$b,$f,$e2) = @{ ELLIPSOIDS->{$shape} }; |
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174
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397
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208
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209
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174
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400
|
my $n = ($a-$b)/($a+$b); |
210
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174
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308
|
my $af = $a * CONVERGENCE_FACTOR; |
211
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212
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174
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264
|
my $phi = $lat / 57.29577951308232087679815481410517; |
213
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174
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300
|
my $lam = $lon / 57.29577951308232087679815481410517; |
214
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215
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174
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376
|
my $cp = cos $phi; my $sp = sin $phi; |
|
174
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284
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216
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174
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269
|
my $sp2 = $sp*$sp; |
217
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174
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274
|
my $tp = $sp/$cp; # cos phi cannot be zero in GB |
218
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174
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224
|
my $tp2 = $tp*$tp; |
219
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174
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284
|
my $tp4 = $tp2*$tp2; |
220
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221
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174
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298
|
my $splat = 1 - $e2 * $sp2; |
222
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174
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253
|
my $sqrtsplat = sqrt $splat; |
223
|
174
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283
|
my $nu = $af / $sqrtsplat; |
224
|
174
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304
|
my $rho = $af * (1 - $e2) / ($splat*$sqrtsplat); |
225
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174
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269
|
my $eta2 = $nu/$rho - 1; |
226
|
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227
|
174
|
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270
|
my $p_plus = $phi + ORIGIN_LATITUDE; |
228
|
174
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261
|
my $p_minus = $phi - ORIGIN_LATITUDE; |
229
|
174
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832
|
my $M = $b * CONVERGENCE_FACTOR * ( |
230
|
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|
|
(1 + $n * (1 + 5/4*$n*(1 + $n)))*$p_minus |
231
|
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|
|
- 3*$n*(1+$n*(1+7/8*$n)) * sin( $p_minus) * cos( $p_plus) |
232
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|
|
+ (15/8*$n * ($n*(1+$n))) * sin(2*$p_minus) * cos(2*$p_plus) |
233
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|
|
- 35/24*$n**3 * sin(3*$p_minus) * cos(3*$p_plus) |
234
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|
|
); |
235
|
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236
|
174
|
|
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|
|
280
|
my $I = $M + ORIGIN_NORTHING; |
237
|
174
|
|
|
|
|
304
|
my $II = $nu/2 * $sp * $cp; |
238
|
174
|
|
|
|
|
436
|
my $III = $nu/24 * $sp * $cp**3 * (5-$tp2+9*$eta2); |
239
|
174
|
|
|
|
|
390
|
my $IIIA = $nu/720* $sp * $cp**5 *(61-58*$tp2+$tp4); |
240
|
|
|
|
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|
|
|
241
|
174
|
|
|
|
|
235
|
my $IV = $nu*$cp; |
242
|
174
|
|
|
|
|
341
|
my $V = $nu/6 * $cp**3 * ($nu/$rho-$tp2); |
243
|
174
|
|
|
|
|
428
|
my $VI = $nu/120 * $cp**5 * (5-18*$tp2+$tp4+14*$eta2-58*$tp2*$eta2); |
244
|
|
|
|
|
|
|
|
245
|
174
|
|
|
|
|
259
|
my $dl = $lam - ORIGIN_LONGITUDE; |
246
|
174
|
|
|
|
|
344
|
my $north = $I + ( $II + ( $III + $IIIA * $dl * $dl ) * $dl * $dl ) * $dl * $dl; |
247
|
174
|
|
|
|
|
314
|
my $east = ORIGIN_EASTING + ( $IV + ( $V + $VI * $dl * $dl ) * $dl * $dl ) * $dl; |
248
|
|
|
|
|
|
|
|
249
|
174
|
|
|
|
|
465
|
return ($east, $north); |
250
|
|
|
|
|
|
|
} |
251
|
|
|
|
|
|
|
|
252
|
|
|
|
|
|
|
sub _find_OSTN_shifts_at { |
253
|
|
|
|
|
|
|
|
254
|
573
|
|
|
573
|
|
974
|
my ($easting, $northing) = @_; |
255
|
|
|
|
|
|
|
|
256
|
573
|
100
|
|
|
|
1127
|
return if $easting < 0; |
257
|
568
|
100
|
|
|
|
1033
|
return if $easting > 700000; |
258
|
567
|
100
|
|
|
|
1019
|
return if $northing < 0; |
259
|
566
|
100
|
|
|
|
952
|
return if $northing > 1250000; |
260
|
|
|
|
|
|
|
|
261
|
565
|
|
|
|
|
916
|
my $east_km = int($easting / 1000); |
262
|
565
|
|
|
|
|
839
|
my $north_km = int($northing / 1000); |
263
|
|
|
|
|
|
|
|
264
|
565
|
|
|
|
|
1144
|
my $lle = (MIN_EE_SHIFT + $EE_SHIFTS[$east_km + $north_km * 701])/1000; |
265
|
565
|
|
|
|
|
919
|
my $lre = (MIN_EE_SHIFT + $EE_SHIFTS[$east_km + $north_km * 701 + 1])/1000; |
266
|
565
|
|
|
|
|
922
|
my $ule = (MIN_EE_SHIFT + $EE_SHIFTS[$east_km + $north_km * 701 + 701])/1000; |
267
|
565
|
|
|
|
|
922
|
my $ure = (MIN_EE_SHIFT + $EE_SHIFTS[$east_km + $north_km * 701 + 702])/1000; |
268
|
|
|
|
|
|
|
|
269
|
565
|
|
|
|
|
936
|
my $lln = (MIN_NN_SHIFT + $NN_SHIFTS[$east_km + $north_km * 701])/1000; |
270
|
565
|
|
|
|
|
831
|
my $lrn = (MIN_NN_SHIFT + $NN_SHIFTS[$east_km + $north_km * 701 + 1])/1000; |
271
|
565
|
|
|
|
|
913
|
my $uln = (MIN_NN_SHIFT + $NN_SHIFTS[$east_km + $north_km * 701 + 701])/1000; |
272
|
565
|
|
|
|
|
856
|
my $urn = (MIN_NN_SHIFT + $NN_SHIFTS[$east_km + $north_km * 701 + 702])/1000; |
273
|
|
|
|
|
|
|
|
274
|
565
|
|
|
|
|
883
|
my $t = ($easting / 1000) - $east_km; |
275
|
565
|
|
|
|
|
858
|
my $u = ($northing / 1000) - $north_km; |
276
|
|
|
|
|
|
|
|
277
|
|
|
|
|
|
|
return ( |
278
|
565
|
|
|
|
|
1874
|
(1-$t) * (1-$u) * $lle + $t * (1-$u) * $lre + (1-$t) * $u * $ule + $t * $u * $ure, |
279
|
|
|
|
|
|
|
(1-$t) * (1-$u) * $lln + $t * (1-$u) * $lrn + (1-$t) * $u * $uln + $t * $u * $urn |
280
|
|
|
|
|
|
|
); |
281
|
|
|
|
|
|
|
} |
282
|
|
|
|
|
|
|
|
283
|
|
|
|
|
|
|
sub grid_to_ll { |
284
|
|
|
|
|
|
|
|
285
|
147
|
|
|
147
|
1
|
55768
|
my ($e, $n, $options) = @_; |
286
|
|
|
|
|
|
|
|
287
|
147
|
50
|
66
|
|
|
518
|
if (ref $e && defined $e->{e} && defined $e->{n}) { |
|
|
|
66
|
|
|
|
|
288
|
1
|
|
|
|
|
4
|
$options = $e; |
289
|
1
|
|
|
|
|
2
|
$e = $options->{e}; |
290
|
1
|
|
|
|
|
3
|
$n = $options->{n}; |
291
|
|
|
|
|
|
|
} |
292
|
|
|
|
|
|
|
|
293
|
147
|
50
|
|
|
|
465
|
my $shape = exists $options->{shape} ? $options->{shape} : $default_shape; |
294
|
|
|
|
|
|
|
|
295
|
147
|
50
|
|
|
|
446
|
croak "Unknown shape: $shape" if !exists ELLIPSOIDS->{$shape}; |
296
|
|
|
|
|
|
|
|
297
|
147
|
|
|
|
|
449
|
my ($os_lat, $os_lon) = _reverse_project_onto_ellipsoid($e, $n, 'OSGB36'); |
298
|
|
|
|
|
|
|
|
299
|
|
|
|
|
|
|
# if we want OS map LL we are done |
300
|
147
|
100
|
|
|
|
412
|
if ($shape eq 'OSGB36') { |
301
|
6
|
|
|
|
|
67
|
return ($os_lat, $os_lon) |
302
|
|
|
|
|
|
|
} |
303
|
|
|
|
|
|
|
|
304
|
|
|
|
|
|
|
# If we want WGS84 LL, we must adjust to pseudo grid if we can |
305
|
141
|
|
|
|
|
364
|
my ($dx, $dy) = _find_OSTN_shifts_at($e,$n); |
306
|
141
|
50
|
|
|
|
342
|
if ($dx) { |
307
|
141
|
|
|
|
|
231
|
my $in_ostn02_polygon = 1; |
308
|
141
|
|
|
|
|
316
|
my ($x,$y) = ($e-$dx, $n-$dy); |
309
|
141
|
|
|
|
|
293
|
my ($last_dx, $last_dy) = ($dx, $dy); |
310
|
|
|
|
|
|
|
APPROX: |
311
|
141
|
|
|
|
|
363
|
for (1..20) { |
312
|
281
|
|
|
|
|
524
|
($dx, $dy) = _find_OSTN_shifts_at($x,$y); |
313
|
|
|
|
|
|
|
|
314
|
281
|
100
|
|
|
|
588
|
if (!$dx) { |
315
|
|
|
|
|
|
|
# we have been shifted off the edge |
316
|
1
|
|
|
|
|
3
|
$in_ostn02_polygon = 0; |
317
|
|
|
|
|
|
|
last APPROX |
318
|
1
|
|
|
|
|
5
|
} |
319
|
|
|
|
|
|
|
|
320
|
280
|
|
|
|
|
529
|
($x,$y) = ($e-$dx, $n-$dy); |
321
|
280
|
100
|
100
|
|
|
1020
|
last APPROX if abs($dx-$last_dx) < TENTH_MM |
322
|
|
|
|
|
|
|
&& abs($dy-$last_dy) < TENTH_MM; |
323
|
140
|
|
|
|
|
311
|
($last_dx, $last_dy) = ($dx, $dy); |
324
|
|
|
|
|
|
|
} |
325
|
141
|
100
|
|
|
|
335
|
if ($in_ostn02_polygon ) { |
326
|
140
|
|
|
|
|
361
|
return _reverse_project_onto_ellipsoid($e-$dx, $n-$dy, 'WGS84') |
327
|
|
|
|
|
|
|
} |
328
|
|
|
|
|
|
|
} |
329
|
|
|
|
|
|
|
|
330
|
|
|
|
|
|
|
# If we get here, we must use the Helmert approx |
331
|
1
|
|
|
|
|
9
|
return _shift_ll_from_osgb36_to_wgs84($os_lat, $os_lon) |
332
|
|
|
|
|
|
|
} |
333
|
|
|
|
|
|
|
|
334
|
|
|
|
|
|
|
sub grid_to_ll_helmert { |
335
|
3
|
|
|
3
|
1
|
7
|
my ($e, $n) = @_; |
336
|
3
|
|
|
|
|
8
|
my ($os_lat, $os_lon) = _reverse_project_onto_ellipsoid($e, $n, 'OSGB36'); |
337
|
3
|
|
|
|
|
8
|
return _shift_ll_from_osgb36_to_wgs84($os_lat, $os_lon) |
338
|
|
|
|
|
|
|
} |
339
|
|
|
|
|
|
|
|
340
|
|
|
|
|
|
|
sub _reverse_project_onto_ellipsoid { |
341
|
|
|
|
|
|
|
|
342
|
290
|
|
|
290
|
|
562
|
my ( $easting, $northing, $shape ) = @_; |
343
|
|
|
|
|
|
|
|
344
|
290
|
|
|
|
|
421
|
my ( $a, $b, $f, $e2 ) = @{ ELLIPSOIDS->{$shape} }; |
|
290
|
|
|
|
|
771
|
|
345
|
|
|
|
|
|
|
|
346
|
290
|
|
|
|
|
697
|
my $n = ( $a - $b ) / ( $a + $b ); |
347
|
290
|
|
|
|
|
478
|
my $af = $a * CONVERGENCE_FACTOR; |
348
|
|
|
|
|
|
|
|
349
|
290
|
|
|
|
|
495
|
my $dn = $northing - ORIGIN_NORTHING; |
350
|
290
|
|
|
|
|
436
|
my $de = $easting - ORIGIN_EASTING; |
351
|
|
|
|
|
|
|
|
352
|
290
|
|
|
|
|
477
|
my $phi = ORIGIN_LATITUDE + $dn/$af; |
353
|
290
|
|
|
|
|
397
|
my $lam = ORIGIN_LONGITUDE; |
354
|
|
|
|
|
|
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355
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290
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463
|
my ($M, $p_plus, $p_minus); |
356
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290
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|
414
|
while (1) { |
357
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1030
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|
1273
|
$p_plus = $phi + ORIGIN_LATITUDE; |
358
|
1030
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|
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|
1331
|
$p_minus = $phi - ORIGIN_LATITUDE; |
359
|
1030
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3857
|
$M = $b * CONVERGENCE_FACTOR * ( |
360
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(1 + $n * (1 + 5/4*$n*(1 + $n)))*$p_minus |
361
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|
- 3*$n*(1+$n*(1+7/8*$n)) * sin( $p_minus) * cos( $p_plus) |
362
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|
+ (15/8*$n * ($n*(1+$n))) * sin(2*$p_minus) * cos(2*$p_plus) |
363
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|
- 35/24*$n**3 * sin(3*$p_minus) * cos(3*$p_plus) |
364
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|
); |
365
|
1030
|
100
|
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|
2191
|
last if abs($dn-$M) < HUNDREDTH_MM; |
366
|
740
|
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1070
|
$phi = $phi + ($dn-$M)/$af; |
367
|
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|
} |
368
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369
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290
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497
|
my $cp = cos $phi; |
370
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290
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470
|
my $sp = sin $phi; |
371
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290
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448
|
my $tp = $sp / $cp; # cos phi cannot be zero in GB |
372
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373
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290
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500
|
my $splat = 1 - $e2 * $sp * $sp; |
374
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290
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435
|
my $sqrtsplat = sqrt $splat; |
375
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290
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426
|
my $nu = $af / $sqrtsplat; |
376
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290
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512
|
my $rho = $af * (1 - $e2) / ( $splat * $sqrtsplat ); |
377
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290
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506
|
my $eta2 = $nu / $rho - 1; |
378
|
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379
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290
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492
|
my $VII = $tp / (2 * $rho * $nu); |
380
|
290
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|
748
|
my $VIII = $tp / (24 * $rho * $nu**3) * (5 + $eta2 + ( 3 - 9 * $eta2 ) * $tp * $tp ); |
381
|
290
|
|
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|
|
659
|
my $IX = $tp / (720 * $rho * $nu**5) * (61 + ( 90 + 45 * $tp * $tp ) * $tp * $tp ); |
382
|
|
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|
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383
|
290
|
|
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|
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445
|
my $secp = 1/$cp; |
384
|
|
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|
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|
|
385
|
290
|
|
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|
412
|
my $X = $secp / $nu; |
386
|
290
|
|
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|
|
632
|
my $XI = $secp / ( 6 * $nu**3 ) * ( $nu / $rho + 2 * $tp * $tp ); |
387
|
290
|
|
|
|
|
602
|
my $XII = $secp / ( 120 * $nu**5 ) * ( 5 + ( 28 + 24 * $tp * $tp ) * $tp * $tp ); |
388
|
290
|
|
|
|
|
695
|
my $XIIA = $secp / ( 5040 * $nu**7 ) * ( 61 + ( 662 + ( 1320 + 720 * $tp * $tp ) * $tp * $tp ) * $tp * $tp ); |
389
|
|
|
|
|
|
|
|
390
|
290
|
|
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|
|
603
|
$phi = $phi + ( -$VII + ( $VIII - $IX * $de * $de ) * $de * $de) * $de * $de; |
391
|
290
|
|
|
|
|
536
|
$lam = $lam + ( $X + ( -$XI + ( $XII - $XIIA * $de * $de ) * $de * $de) * $de * $de) * $de; |
392
|
|
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393
|
|
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|
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|
|
# now put into degrees & return |
394
|
290
|
|
|
|
|
1241
|
return ($phi * 57.29577951308232087679815481410517, |
395
|
|
|
|
|
|
|
$lam * 57.29577951308232087679815481410517); |
396
|
|
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|
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|
|
} |
397
|
|
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398
|
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1; |
399
|
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400
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|
=pod |
401
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402
|
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|
=head1 NAME |
403
|
|
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404
|
|
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|
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|
|
Geo::Coordinates::OSGB - Convert coordinates between Lat/Lon and the British National Grid |
405
|
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406
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|
An implementation of co-ordinate conversion for England, Wales, and Scotland |
407
|
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|
|
based on formulae and data published by the Ordnance Survey of Great Britain. |
408
|
|
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|
|
409
|
|
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|
|
=head1 VERSION |
410
|
|
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411
|
|
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|
|
2.20 |
412
|
|
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|
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413
|
|
|
|
|
|
|
=for HTML |
414
|
|
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|
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415
|
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416
|
|
|
|
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|
|
=head1 SYNOPSIS |
417
|
|
|
|
|
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|
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418
|
|
|
|
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|
|
use Geo::Coordinates::OSGB qw(ll_to_grid grid_to_ll); |
419
|
|
|
|
|
|
|
|
420
|
|
|
|
|
|
|
($easting,$northing) = ll_to_grid($lat,$lon); |
421
|
|
|
|
|
|
|
($lat,$lon) = grid_to_ll($easting,$northing); |
422
|
|
|
|
|
|
|
|
423
|
|
|
|
|
|
|
=head1 DESCRIPTION |
424
|
|
|
|
|
|
|
|
425
|
|
|
|
|
|
|
These modules convert accurately between OSGB national grid references and |
426
|
|
|
|
|
|
|
coordinates given in latitude and longitude. |
427
|
|
|
|
|
|
|
|
428
|
|
|
|
|
|
|
The default "ellipsoid model" used for the conversions is the I |
429
|
|
|
|
|
|
|
international standard WGS84. This means that you can take latitude and |
430
|
|
|
|
|
|
|
longitude readings from your GPS receiver, or read them from Wikipedia, or |
431
|
|
|
|
|
|
|
Google Earth, or your car's sat-nav, and use this module to convert them to |
432
|
|
|
|
|
|
|
accurate British National grid references for use with one of the Ordnance |
433
|
|
|
|
|
|
|
Survey's paper maps. And I, of course. |
434
|
|
|
|
|
|
|
|
435
|
|
|
|
|
|
|
The module is implemented purely in Perl, and should run on any platform with |
436
|
|
|
|
|
|
|
Perl version 5.8 or better. |
437
|
|
|
|
|
|
|
|
438
|
|
|
|
|
|
|
In this description, the abbreviations `OS' and `OSGB' mean `the Ordnance |
439
|
|
|
|
|
|
|
Survey of Great Britain': the British government agency that produces the |
440
|
|
|
|
|
|
|
standard maps of England, Wales, and Scotland. Any mention of `sheets' or |
441
|
|
|
|
|
|
|
`maps' refers to one or more of the map sheets defined in the accompanying maps |
442
|
|
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|
|
|
|
module. |
443
|
|
|
|
|
|
|
|
444
|
|
|
|
|
|
|
This code is written for the British national grid system. It is of no use |
445
|
|
|
|
|
|
|
outside Britain. In fact it's only really useful in the areas covered by the |
446
|
|
|
|
|
|
|
OS's main series of maps, which exclude the Channel Islands and Northern |
447
|
|
|
|
|
|
|
Ireland. |
448
|
|
|
|
|
|
|
|
449
|
|
|
|
|
|
|
=head1 SUBROUTINES/METHODS |
450
|
|
|
|
|
|
|
|
451
|
|
|
|
|
|
|
The following functions can be exported from the |
452
|
|
|
|
|
|
|
C module: |
453
|
|
|
|
|
|
|
|
454
|
|
|
|
|
|
|
grid_to_ll |
455
|
|
|
|
|
|
|
ll_to_grid |
456
|
|
|
|
|
|
|
|
457
|
|
|
|
|
|
|
Neither of these is exported by default. |
458
|
|
|
|
|
|
|
|
459
|
|
|
|
|
|
|
=head2 Main subroutines |
460
|
|
|
|
|
|
|
|
461
|
|
|
|
|
|
|
=head3 C |
462
|
|
|
|
|
|
|
|
463
|
|
|
|
|
|
|
C translates a latitude and longitude pair into a grid |
464
|
|
|
|
|
|
|
easting and northing pair. |
465
|
|
|
|
|
|
|
|
466
|
|
|
|
|
|
|
When called in a list context, C returns the easting and |
467
|
|
|
|
|
|
|
northing as a list of two. When called in a scalar context, it returns |
468
|
|
|
|
|
|
|
a single string with the numbers separated by a space. |
469
|
|
|
|
|
|
|
|
470
|
|
|
|
|
|
|
The arguments should be supplied as real numbers representing |
471
|
|
|
|
|
|
|
decimal degrees, like this: |
472
|
|
|
|
|
|
|
|
473
|
|
|
|
|
|
|
my ($e,$n) = ll_to_grid(51.5, -2.1); # (393154.801, 177900.605) |
474
|
|
|
|
|
|
|
|
475
|
|
|
|
|
|
|
Following the normal mathematical convention, positive arguments mean North or |
476
|
|
|
|
|
|
|
East, negative South or West. |
477
|
|
|
|
|
|
|
|
478
|
|
|
|
|
|
|
If you have data with degrees, minutes, and seconds, you can convert them |
479
|
|
|
|
|
|
|
to decimals like this: |
480
|
|
|
|
|
|
|
|
481
|
|
|
|
|
|
|
my ($e,$n) = ll_to_grid(51+25/60, 0-5/60-2/3600); |
482
|
|
|
|
|
|
|
|
483
|
|
|
|
|
|
|
If you have trouble remembering the order of the arguments, or the returned |
484
|
|
|
|
|
|
|
values, note that latitude comes before longitude in the alphabet too, as |
485
|
|
|
|
|
|
|
easting comes before northing. However, since reasonable latitudes for the |
486
|
|
|
|
|
|
|
OSGB are in the range 49 to 61, and reasonable longitudes in the range -9 to |
487
|
|
|
|
|
|
|
+2, C accepts the arguments in either order; if your longitude is |
488
|
|
|
|
|
|
|
larger than your latitude, then the values of the arguments will be silently |
489
|
|
|
|
|
|
|
swapped. |
490
|
|
|
|
|
|
|
|
491
|
|
|
|
|
|
|
You can also supply the arguments as named keywords (but be sure to use |
492
|
|
|
|
|
|
|
the curly braces so that you pass them as a reference): |
493
|
|
|
|
|
|
|
|
494
|
|
|
|
|
|
|
my ($e,$n) = ll_to_grid( { lat => 51.5, lon => -2.1 } ); |
495
|
|
|
|
|
|
|
|
496
|
|
|
|
|
|
|
The easting and northing will be returned as the orthogonal distances in metres |
497
|
|
|
|
|
|
|
from the `false point of origin' of the British Grid (which is a point some way |
498
|
|
|
|
|
|
|
to the south-west of the Scilly Isles). The returned pair refers to a point on |
499
|
|
|
|
|
|
|
the usual OSGB grid, which extends from the Scilly Isles in the south west to |
500
|
|
|
|
|
|
|
the Shetlands in the north. |
501
|
|
|
|
|
|
|
|
502
|
|
|
|
|
|
|
my ($e,$n) = ll_to_grid(51.5, -2.1); # (393154.807, 177900.595) |
503
|
|
|
|
|
|
|
my $s = ll_to_grid(51.5, -2.1); # "393154.807 177900.595" |
504
|
|
|
|
|
|
|
|
505
|
|
|
|
|
|
|
If the coordinates you supply are in the area covered by the OSTN |
506
|
|
|
|
|
|
|
transformation data, then the results will be rounded to 3 decimal places, |
507
|
|
|
|
|
|
|
which corresponds to the nearest millimetre. If they are outside the coverage |
508
|
|
|
|
|
|
|
then the conversion is automagically done using a Helmert transformation |
509
|
|
|
|
|
|
|
instead of the OSTN data. The results will be rounded to the nearest metre |
510
|
|
|
|
|
|
|
in this case, although you probably should not rely on the results being more |
511
|
|
|
|
|
|
|
accurate than about 5m. |
512
|
|
|
|
|
|
|
|
513
|
|
|
|
|
|
|
With the older OSTN02 dataset, coverage extended only to about 3km offshore, |
514
|
|
|
|
|
|
|
but the current OSTN15 dataset extends coverage to the whole grid area |
515
|
|
|
|
|
|
|
from (0,0) to (700000, 1250000), so you have be really far away to get |
516
|
|
|
|
|
|
|
whole metres. Even points well away from land, like this one: |
517
|
|
|
|
|
|
|
|
518
|
|
|
|
|
|
|
# A point in the sea, to the north-west of Coll |
519
|
|
|
|
|
|
|
my $s = ll_to_grid(56.75,-7); |
520
|
|
|
|
|
|
|
|
521
|
|
|
|
|
|
|
will get an accurate conversion. With OSTN02 that returned C<94471 773206> |
522
|
|
|
|
|
|
|
but with OSTN15 you get C<94469.597 773209.464>. For your sake, I hope you are |
523
|
|
|
|
|
|
|
never in a situation at sea off Coll where the 3 metres difference is important. |
524
|
|
|
|
|
|
|
|
525
|
|
|
|
|
|
|
The numbers returned may be negative if your latitude and longitude are |
526
|
|
|
|
|
|
|
far enough south and west, but beware that the transformation is less |
527
|
|
|
|
|
|
|
and less accurate or useful the further you get from the British Isles. |
528
|
|
|
|
|
|
|
|
529
|
|
|
|
|
|
|
If you want the result presented in a more traditional grid reference |
530
|
|
|
|
|
|
|
format you should pass the results to one of the grid formatting |
531
|
|
|
|
|
|
|
routines from L. Like this. |
532
|
|
|
|
|
|
|
|
533
|
|
|
|
|
|
|
my $s = ll_to_grid(51.5, -2.1); # "393154.807 177900.595" |
534
|
|
|
|
|
|
|
$s = format_grid(ll_to_grid(51.5,-2.1)); # "ST 931 779" |
535
|
|
|
|
|
|
|
$s = format_grid_GPS(ll_to_grid(51.5,-2.1)); # "ST 93154 77900" |
536
|
|
|
|
|
|
|
$s = format_grid_map(ll_to_grid(51.5,-2.1)); # "ST 931 779 on A:173, B:156, C:157" |
537
|
|
|
|
|
|
|
|
538
|
|
|
|
|
|
|
C also takes an optional argument that sets the ellipsoid |
539
|
|
|
|
|
|
|
model to use. This defaults to `WGS84', the name of the normal model |
540
|
|
|
|
|
|
|
for working with normal GPS coordinates, but if you want to work with |
541
|
|
|
|
|
|
|
the traditional latitude and longitude values printed around the edges of |
542
|
|
|
|
|
|
|
OS maps before 2015 then you should add an optional shape parameter like this: |
543
|
|
|
|
|
|
|
|
544
|
|
|
|
|
|
|
my ($e, $n) = ll_to_grid(49,-2, {shape => 'OSGB36'}); |
545
|
|
|
|
|
|
|
|
546
|
|
|
|
|
|
|
Incidentally, if you make this call above you will get back |
547
|
|
|
|
|
|
|
C<(400000, -100000)> which are the coordinates of the `true point of origin' |
548
|
|
|
|
|
|
|
of the British grid. You should get back an easting of 400000 for any |
549
|
|
|
|
|
|
|
point with longitude 2W since this is the central meridian used for the |
550
|
|
|
|
|
|
|
OSGB projection. However you will get a slightly different value unless |
551
|
|
|
|
|
|
|
you specify C<< {shape => 'OSGB36'} >> because the WGS84 meridians are not |
552
|
|
|
|
|
|
|
quite the same as OSGB36. |
553
|
|
|
|
|
|
|
|
554
|
|
|
|
|
|
|
=head3 C |
555
|
|
|
|
|
|
|
|
556
|
|
|
|
|
|
|
The routine C takes an easting and northing pair |
557
|
|
|
|
|
|
|
representing the distance in metres from the `false point of origin' of |
558
|
|
|
|
|
|
|
the OSGB grid and returns a pair of real numbers representing the |
559
|
|
|
|
|
|
|
equivalent longitude and latitude coordinates in the WGS84 model. |
560
|
|
|
|
|
|
|
|
561
|
|
|
|
|
|
|
Following convention, positive results are North of the equator and East |
562
|
|
|
|
|
|
|
of the prime meridian, negative numbers are South and West. The |
563
|
|
|
|
|
|
|
fractional parts of the results represent decimal fractions of degrees. |
564
|
|
|
|
|
|
|
|
565
|
|
|
|
|
|
|
No special processing is done in scalar context because there is no |
566
|
|
|
|
|
|
|
obvious assumption about how to round the results. You will just get |
567
|
|
|
|
|
|
|
the length of the list returned, which is 2. |
568
|
|
|
|
|
|
|
|
569
|
|
|
|
|
|
|
The arguments must be an (easting, northing) pair representing the |
570
|
|
|
|
|
|
|
absolute grid reference in metres from the point of origin. You can get |
571
|
|
|
|
|
|
|
these from a traditional grid reference string by calling |
572
|
|
|
|
|
|
|
C first. |
573
|
|
|
|
|
|
|
|
574
|
|
|
|
|
|
|
my ($lat, $lon) = grid_to_ll(parse_grid('SM 349 231')) |
575
|
|
|
|
|
|
|
|
576
|
|
|
|
|
|
|
An optional last argument defines the ellipsoid model to use just as it |
577
|
|
|
|
|
|
|
does for C. This is only necessary is you are working |
578
|
|
|
|
|
|
|
with an ellipsoid model other than WGS84. Pass the argument as a hash |
579
|
|
|
|
|
|
|
ref with a `shape' key. |
580
|
|
|
|
|
|
|
|
581
|
|
|
|
|
|
|
my ($lat, $lon) = grid_to_ll(400000, 300000, {shape => 'OSGB36'}); |
582
|
|
|
|
|
|
|
|
583
|
|
|
|
|
|
|
If you like named arguments then you can use a single hash ref for all |
584
|
|
|
|
|
|
|
of them (this is strictly optional): |
585
|
|
|
|
|
|
|
|
586
|
|
|
|
|
|
|
my ($lat, $lon) = grid_to_ll({ e => 400000, n => 300000, shape => 'OSGB36'}); |
587
|
|
|
|
|
|
|
|
588
|
|
|
|
|
|
|
The results returned will be floating point numbers with the default |
589
|
|
|
|
|
|
|
Perl precision. Unless you are running with long double precision |
590
|
|
|
|
|
|
|
floats you will get 13 decimal places for latitude and 14 places for |
591
|
|
|
|
|
|
|
longitude; but this does not mean that the calculations are accurate to |
592
|
|
|
|
|
|
|
that many places. The OS online conversion tools return decimal degrees |
593
|
|
|
|
|
|
|
to only 6 places. A difference of 1 in the sixth decimal place |
594
|
|
|
|
|
|
|
represents a distance on the ground of about 10 cm. This is probably a |
595
|
|
|
|
|
|
|
good rule of thumb for the reliability of these calculations, but all |
596
|
|
|
|
|
|
|
the available decimal places are returned so that you can choose the |
597
|
|
|
|
|
|
|
rounding that is appropriate for your application. Here's one way to do |
598
|
|
|
|
|
|
|
that: |
599
|
|
|
|
|
|
|
|
600
|
|
|
|
|
|
|
my ($lat, $lon) = map { sprintf "%.6f", $_ } grid_to_ll(431234, 312653); |
601
|
|
|
|
|
|
|
|
602
|
|
|
|
|
|
|
|
603
|
|
|
|
|
|
|
=head2 Additional subroutines |
604
|
|
|
|
|
|
|
|
605
|
|
|
|
|
|
|
=head3 C |
606
|
|
|
|
|
|
|
|
607
|
|
|
|
|
|
|
The default ellipsoid shape used for conversion to and from latitude and |
608
|
|
|
|
|
|
|
longitude is `WGS84' as used in the international GPS system. This |
609
|
|
|
|
|
|
|
default is set every time that you load the module. If you want to |
610
|
|
|
|
|
|
|
process or produce a large number latitude and longitude coordinates in |
611
|
|
|
|
|
|
|
the British Ordnance Survey system (as printed round the edges of OS |
612
|
|
|
|
|
|
|
Landranger and Explorer maps before 2015) you can use C<< set_default_shape('OSGB36'); >> to |
613
|
|
|
|
|
|
|
set the default shape to OSGB36. This saves you having to add C<< { |
614
|
|
|
|
|
|
|
shape => 'OSGB36' } >> to every call of C or C. |
615
|
|
|
|
|
|
|
|
616
|
|
|
|
|
|
|
You can use C<< set_default_shape('WGS84'); >> to set the default shape back |
617
|
|
|
|
|
|
|
to WGS84 again when finished with OSGB36 coordinates. |
618
|
|
|
|
|
|
|
|
619
|
|
|
|
|
|
|
=head3 C |
620
|
|
|
|
|
|
|
|
621
|
|
|
|
|
|
|
You can use this function to do a conversion from WGS84 lat/lon |
622
|
|
|
|
|
|
|
to the OS grid without using the whole OSTN data set. The algorithm |
623
|
|
|
|
|
|
|
used is known as a Helmert transformation. This is the usual coordinate |
624
|
|
|
|
|
|
|
conversion algorithm implemented in most consumer-level GPS devices, which |
625
|
|
|
|
|
|
|
generally do not have enough memory space for the whole of OSTN. It |
626
|
|
|
|
|
|
|
is based on parameters supplied by the OS; they suggest that in most of |
627
|
|
|
|
|
|
|
the UK this conversion is accurate to within about 5m. |
628
|
|
|
|
|
|
|
|
629
|
|
|
|
|
|
|
my ($e, $n) = ll_to_grid_helmert(51.477811, -0.001475); # RO Greenwich |
630
|
|
|
|
|
|
|
|
631
|
|
|
|
|
|
|
The input must be decimal degrees in the WGS84 model, with latitude |
632
|
|
|
|
|
|
|
first and longitude second. The results are rounded to the nearest |
633
|
|
|
|
|
|
|
whole metre. They can be used with C in the same way as |
634
|
|
|
|
|
|
|
the results from C. |
635
|
|
|
|
|
|
|
|
636
|
|
|
|
|
|
|
This function is called automatically by C if your |
637
|
|
|
|
|
|
|
coordinates are WGS84 and lie outside the OSTN polygon. |
638
|
|
|
|
|
|
|
|
639
|
|
|
|
|
|
|
=head3 C |
640
|
|
|
|
|
|
|
|
641
|
|
|
|
|
|
|
You can use this function to do a slightly quicker conversion from OS grid |
642
|
|
|
|
|
|
|
references to WGS84 latitude and longitude coordinates without using the |
643
|
|
|
|
|
|
|
whole OSTN data set. The algorithm used is known as a Helmert |
644
|
|
|
|
|
|
|
transformation. This is the usual coordinate conversion algorithm |
645
|
|
|
|
|
|
|
implemented in most consumer-level GPS devices. It is based on |
646
|
|
|
|
|
|
|
parameters supplied by the OS; they suggest that in most of the UK this |
647
|
|
|
|
|
|
|
conversion is accurate to within about 5m. |
648
|
|
|
|
|
|
|
|
649
|
|
|
|
|
|
|
my ($lat, $lon) = grid_to_ll_helmert(538885, 177322); |
650
|
|
|
|
|
|
|
|
651
|
|
|
|
|
|
|
The input must be in metres from false point of origin (as produced by |
652
|
|
|
|
|
|
|
C) and the results are in decimal degrees using the WGS84 |
653
|
|
|
|
|
|
|
model. |
654
|
|
|
|
|
|
|
|
655
|
|
|
|
|
|
|
The results are returned with the full Perl precision in the same way as |
656
|
|
|
|
|
|
|
C so that you can choose an appropriate rounding for your |
657
|
|
|
|
|
|
|
needs. Four or five decimal places is probably appropriate in most |
658
|
|
|
|
|
|
|
cases. This represents somewhere between 1 and 10 m on the ground. |
659
|
|
|
|
|
|
|
|
660
|
|
|
|
|
|
|
This function is called automatically by C if the grid reference |
661
|
|
|
|
|
|
|
you supply lies outside the OSTN polygon. (All such spots are far out to sea). |
662
|
|
|
|
|
|
|
The results are only useful close to mainland Britain. |
663
|
|
|
|
|
|
|
|
664
|
|
|
|
|
|
|
=head3 Importing all the functions |
665
|
|
|
|
|
|
|
|
666
|
|
|
|
|
|
|
You can import all the functions defined in C with an C<:all> tag. |
667
|
|
|
|
|
|
|
|
668
|
|
|
|
|
|
|
use Geo::Coordinates::OSGB ':all'; |
669
|
|
|
|
|
|
|
|
670
|
|
|
|
|
|
|
=head1 EXAMPLES |
671
|
|
|
|
|
|
|
|
672
|
|
|
|
|
|
|
use Geo::Coordinates::OSGB qw/ll_to_grid grid_to_ll/; |
673
|
|
|
|
|
|
|
|
674
|
|
|
|
|
|
|
# Latitude and longitude according to the WGS84 model |
675
|
|
|
|
|
|
|
($lat, $lon) = grid_to_ll($e, $n); |
676
|
|
|
|
|
|
|
|
677
|
|
|
|
|
|
|
# and to go the other way |
678
|
|
|
|
|
|
|
($e, $n) = ll_to_grid($lat,$lon); |
679
|
|
|
|
|
|
|
|
680
|
|
|
|
|
|
|
See the test files for more examples of usage. |
681
|
|
|
|
|
|
|
|
682
|
|
|
|
|
|
|
=head1 BUGS AND LIMITATIONS |
683
|
|
|
|
|
|
|
|
684
|
|
|
|
|
|
|
The formulae supplied by the OS and used for the conversion routines are |
685
|
|
|
|
|
|
|
specifically designed to be close floating-point approximations rather |
686
|
|
|
|
|
|
|
than exact mathematical equivalences. So after round-trips like these: |
687
|
|
|
|
|
|
|
|
688
|
|
|
|
|
|
|
($lat1,$lon1) = grid_to_ll(ll_to_grid($lat0,$lon0)); |
689
|
|
|
|
|
|
|
($e1,$n1) = ll_to_grid(grid_to_ll($e0,$n0)); |
690
|
|
|
|
|
|
|
|
691
|
|
|
|
|
|
|
neither C<$lat1 == $lat0> nor C<$lon1 == $lon0> nor C<$e1 == $e0> nor |
692
|
|
|
|
|
|
|
C<$n1 == $n0> exactly. However the differences should be very small. |
693
|
|
|
|
|
|
|
|
694
|
|
|
|
|
|
|
The OS formulae were designed to give an accuracy of about 1 mm of |
695
|
|
|
|
|
|
|
error. This means that you can rely on the third decimal place for grid |
696
|
|
|
|
|
|
|
references and about the seventh or eighth for latitude and longitude |
697
|
|
|
|
|
|
|
(although the OS themselves only provide six decimal places in their |
698
|
|
|
|
|
|
|
results). |
699
|
|
|
|
|
|
|
|
700
|
|
|
|
|
|
|
For all of England, Wales, Scotland, and the Isle of Man the error will be |
701
|
|
|
|
|
|
|
tiny. All other areas, like Northern Ireland, the Channel Islands or Rockall, |
702
|
|
|
|
|
|
|
and any areas of sea more than a few miles off shore, are outside the coverage |
703
|
|
|
|
|
|
|
of OSTN, so the simpler, less accurate transformation is used. The OS state |
704
|
|
|
|
|
|
|
that this is accurate to about 5m but that the parameters used are only valid |
705
|
|
|
|
|
|
|
in the reasonably close vicinity of the British Isles. |
706
|
|
|
|
|
|
|
|
707
|
|
|
|
|
|
|
Not enough testing has been done. I am always grateful for the feedback |
708
|
|
|
|
|
|
|
I get from users, but especially for problem reports that help me to |
709
|
|
|
|
|
|
|
make this a better module. |
710
|
|
|
|
|
|
|
|
711
|
|
|
|
|
|
|
=head1 DIAGNOSTICS |
712
|
|
|
|
|
|
|
|
713
|
|
|
|
|
|
|
The only error message you will get from this module is about the |
714
|
|
|
|
|
|
|
ellipsoid shape used for the transformation. If you try to set C<< |
715
|
|
|
|
|
|
|
{shape => 'blah'} >> the module will croak with a message saying |
716
|
|
|
|
|
|
|
C. The shape should be one of the shapes defined: |
717
|
|
|
|
|
|
|
WGS84 or OSGB36. |
718
|
|
|
|
|
|
|
|
719
|
|
|
|
|
|
|
Should this software not do what you expect, then please first read this |
720
|
|
|
|
|
|
|
documentation, secondly verify that you have installed it correctly and |
721
|
|
|
|
|
|
|
that it passes all the installation tests on your set up, thirdly study |
722
|
|
|
|
|
|
|
the source code to see what it's supposed to be doing, fourthly get in |
723
|
|
|
|
|
|
|
touch to ask me about it. |
724
|
|
|
|
|
|
|
|
725
|
|
|
|
|
|
|
=head1 CONFIGURATION AND ENVIRONMENT |
726
|
|
|
|
|
|
|
|
727
|
|
|
|
|
|
|
There is no configuration required either of these modules or your |
728
|
|
|
|
|
|
|
environment. It should work on any recent version of Perl, on any |
729
|
|
|
|
|
|
|
platform. |
730
|
|
|
|
|
|
|
|
731
|
|
|
|
|
|
|
=head1 DEPENDENCIES |
732
|
|
|
|
|
|
|
|
733
|
|
|
|
|
|
|
Perl 5.10 or better. |
734
|
|
|
|
|
|
|
|
735
|
|
|
|
|
|
|
=head1 INCOMPATIBILITIES |
736
|
|
|
|
|
|
|
|
737
|
|
|
|
|
|
|
None known. |
738
|
|
|
|
|
|
|
|
739
|
|
|
|
|
|
|
=head1 LICENSE AND COPYRIGHT |
740
|
|
|
|
|
|
|
|
741
|
|
|
|
|
|
|
Copyright (C) 2002-2017 Toby Thurston |
742
|
|
|
|
|
|
|
|
743
|
|
|
|
|
|
|
OSTN transformation data included in this module is freely available |
744
|
|
|
|
|
|
|
from the Ordnance Survey but remains Crown Copyright (C) 2002 |
745
|
|
|
|
|
|
|
|
746
|
|
|
|
|
|
|
This program is free software; you can redistribute it and/or modify it |
747
|
|
|
|
|
|
|
under the terms of the GNU General Public License as published by the |
748
|
|
|
|
|
|
|
Free Software Foundation; either version 2 of the License, or (at your |
749
|
|
|
|
|
|
|
option) any later version. |
750
|
|
|
|
|
|
|
|
751
|
|
|
|
|
|
|
This program is distributed in the hope that it will be useful, but |
752
|
|
|
|
|
|
|
WITHOUT ANY WARRANTY; without even the implied warranty of |
753
|
|
|
|
|
|
|
MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the GNU |
754
|
|
|
|
|
|
|
General Public License for more details. |
755
|
|
|
|
|
|
|
|
756
|
|
|
|
|
|
|
You should have received a copy of the GNU General Public License along |
757
|
|
|
|
|
|
|
with this program; if not, write to the Free Software Foundation, Inc., |
758
|
|
|
|
|
|
|
51 Franklin Street, Fifth Floor, Boston, MA 02110-1301 USA. |
759
|
|
|
|
|
|
|
|
760
|
|
|
|
|
|
|
=head1 AUTHOR |
761
|
|
|
|
|
|
|
|
762
|
|
|
|
|
|
|
Toby Thurston -- 29 Oct 2017 |
763
|
|
|
|
|
|
|
|
764
|
|
|
|
|
|
|
toby@cpan.org |
765
|
|
|
|
|
|
|
|
766
|
|
|
|
|
|
|
=head1 SEE ALSO |
767
|
|
|
|
|
|
|
|
768
|
|
|
|
|
|
|
See L for routines to format grid references. |
769
|
|
|
|
|
|
|
|
770
|
|
|
|
|
|
|
The UK Ordnance Survey's explanations on their web pages. |
771
|
|
|
|
|
|
|
|
772
|
|
|
|
|
|
|
See L for a general approach (not based on the OSGB). |
773
|
|
|
|
|
|
|
|
774
|
|
|
|
|
|
|
=cut |
775
|
|
|
|
|
|
|
|