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  2. Vincenty's formulae - Wikipedia

    en.wikipedia.org/wiki/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 that assume a spherical Earth, such ...

  3. Geodesics on an ellipsoid - Wikipedia

    en.wikipedia.org/wiki/Geodesics_on_an_ellipsoid

    the inverse geodesic problem or second geodesic problem, given A and B, determine s 12, α 1, and α 2. As can be seen from Fig. 1, these problems involve solving the triangle NAB given one angle, α 1 for the direct problem and λ 12 = λ 2 − λ 1 for the inverse problem, and its two adjacent sides.

  4. Thaddeus Vincenty - Wikipedia

    en.wikipedia.org/wiki/Thaddeus_Vincenty

    Thaddeus Vincenty (born Tadeusz Szpila; 27 October 1920 – 6 March 2002) was a Polish American geodesist who worked with the U.S. Air Force and later the National Geodetic Survey to adapt three-dimensional adjustment techniques to NAD 83. [1] He devised Vincenty's formulae, a geodesic calculation technique published in 1975 which is accurate ...

  5. Geographical distance - Wikipedia

    en.wikipedia.org/wiki/Geographical_distance

    Finding the geodesic between two points on the Earth, the so-called inverse geodetic problem, was the focus of many mathematicians and geodesists over the course of the 18th and 19th centuries with major contributions by Clairaut, [5] Legendre, [6] Bessel, [7] and Helmert English translation of Astron. Nachr. 4, 241–254 (1825).

  6. Inverse problem - Wikipedia

    en.wikipedia.org/wiki/Inverse_problem

    An inverse problem in science is the process of calculating from a set of observations the causal factors that produced them: for example, calculating an image in X-ray computed tomography, source reconstruction in acoustics, or calculating the density of the Earth from measurements of its gravity field. It is called an inverse problem because ...

  7. Azimuth - Wikipedia

    en.wikipedia.org/wiki/Azimuth

    The opposite problem occurs when the coordinates (X 1, Y 1) of one point, the distance D, and the azimuth α to another point (X 2, Y 2) are known, one can calculate its coordinates: X 2 = X 1 + D sin ⁡ α Y 2 = Y 1 + D cos ⁡ α {\displaystyle {\begin{aligned}X_{2}&=X_{1}+D\sin \alpha \\Y_{2}&=Y_{1}+D\cos \alpha \end{aligned}}}

  8. Vincenty - Wikipedia

    en.wikipedia.org/wiki/Vincenty

    Vincenty's formulae, a fast algorithm to calculate the distance between two latitude/longitude points Topics referred to by the same term This disambiguation page lists articles associated with the title Vincenty .

  9. Talk:Vincenty's formulae - Wikipedia

    en.wikipedia.org/wiki/Talk:Vincenty's_formulae

    "Nearly antipodal points" which describes the problems of failure to converge or slow convergence for the inverse method. This includes pointers to Vincenty's efforts to correct these problems. I also include a plug for my method of solving the inverse problem via Newton's method because