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Vincenty's formulae : ウィキペディア英語版
Vincenty's formulae

Vincenty's formulae are two related iterative methods used in geodesy to calculate the distance between two points on the surface of a spheroid, developed by Thaddeus Vincenty (1975a) They are based on the assumption that the figure of the Earth is an oblate spheroid, and hence are more accurate than methods such as great-circle distance which assume a spherical Earth.
The first (direct) method computes the location of a point which is a given distance and azimuth (direction) from another point. The second (inverse) method computes the geographical distance and azimuth between two given points. They have been widely used in geodesy because they are accurate to within 0.5 mm (0.020″) on the Earth ellipsoid.
== Background ==

Vincenty's goal was to express existing algorithms for geodesics on an ellipsoid
in a form that minimized the program length
(see the first sentence of his paper). His unpublished report (1975b)
mentions the use of a Wang
720 desk calculator which had only a few
kilobytes of memory. To obtain good accuracy for long lines, the
solution uses the classical solution of Legendre (1806), Bessel (1825),
and Helmert (1880) based on the auxiliary sphere. (Vincenty relied on
formulation of this method given by Rainsford, 1955.) Legendre showed
that an ellipsoidal geodesic can be exactly mapped to a great circle on
the auxiliary sphere by mapping the geographic latitude to reduced
latitude and setting the azimuth of the great circle equal to that of
the geodesic. The longitude on the ellipsoid and the distance along the
geodesic are then given in terms of the longitude on the sphere and the
arc length along the great circle by simple integrals. Bessel and
Helmert gave rapidly converging series for these integrals which allow
the geodesic to be computed with arbitrary accuracy.
In order to minimize the program size, Vincenty took these series,
re-expanded them using the first term of each series as the small
parameter, and truncated them to order ''ƒ''3. This resulted in
compact expressions for the longitude and distance integrals.
The expressions were put in Horner
(or ''nested'') form, since this
allows polynomials to be evaluated using only a single temporary
register. Finally, simple iterative techniques were used
to solve the implicit equations in the direct and inverse methods; even
though these are slow (and in the case of the inverse method it sometimes does
not converge), they result in the least increase in code size.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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