The shortest distance between two points (i.e., the 'great-circle-distance' or 'as the crow flies'), according to the 'Vincenty (ellipsoid)' method. This method uses an ellipsoid and the results are very accurate. The method is computationally more intensive than the other great-circled methods in this package.
1.1
p1: longitude/latitude of point(s), in degrees 1; can be a vector of two numbers, a matrix of 2 columns (first one is longitude, second is latitude) or a SpatialPoints* object
p2: as above; or missing, in which case the sequential distance between the points in p1 is computed
a: Equatorial axis of ellipsoid
b: Polar axis of ellipsoid
f: Inverse flattening of ellipsoid
Details
The WGS84 ellipsoid is used by default. It is the best available global ellipsoid, but for some areas other ellipsoids could be preferable, or even necessary if you work with a printed map that refers to that ellipsoid. Here are parameters for some commonly used ellipsoids:
ellipsoid
a
b
f
WGS84
6378137
6356752.3142
1/298.257223563
GRS80
6378137
6356752.3141
1/298.257222101
GRS67
6378160
6356774.719
1/298.25
Airy 1830
6377563.396
6356256.909
1/299.3249646
Bessel 1841
6377397.155
6356078.965
1/299.1528434
Clarke 1880
6378249.145
6356514.86955
1/293.465
Clarke 1866
6378206.4
6356583.8
1/294.9786982
International 1924
6378388
6356911.946
1/297
Krasovsky 1940
6378245
6356863
1/298.2997381
a is the 'semi-major axis', and b is the 'semi-minor axis' of the ellipsoid. f is the flattening. Note that f = (a-b)/a
Distance value in the same units as the ellipsoid (default is meters)
References
Vincenty, T. 1975. Direct and inverse solutions of geodesics on the ellipsoid with application of nested equations. Survey Review Vol. 23, No. 176, pp88-93. Available here:
distVincentyEllipsoid(c(0,0),c(90,90))# on a 'Clarke 1880' ellipsoiddistVincentyEllipsoid(c(0,0),c(90,90), a=6378249.145, b=6356514.86955, f=1/293.465)