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A circle of radius a compressed to an ellipse.
A sphere of radius a compressed to an oblate ellipsoid of revolution.

Flattening is a measure of the compression of a circle or sphere along a diameter to form an ellipse or an ellipsoid of revolution ( spheroid) respectively. Other terms used are ellipticity, or oblateness. The usual notation for flattening is and its definition in terms of the semi-axes and of the resulting ellipse or ellipsoid is

The compression factor is in each case; for the ellipse, this is also its aspect ratio.

Definitions

There are three variants: the flattening [1] sometimes called the first flattening, [2] as well as two other "flattenings" and each sometimes called the second flattening, [3] sometimes only given a symbol, [4] or sometimes called the second flattening and third flattening, respectively. [5]

In the following, is the larger dimension (e.g. semimajor axis), whereas is the smaller (semiminor axis). All flattenings are zero for a circle (a = b).

(First) flattening  Fundamental. Geodetic reference ellipsoids are specified by giving
Second flattening Rarely used.
Third flattening  Used in geodetic calculations as a small expansion parameter. [6]

Identities

The flattenings can be related to each-other:

The flattenings are related to other parameters of the ellipse. For example,

where is the eccentricity.

See also

References

  1. ^ Snyder, John P. (1987). Map Projections: A Working Manual. U.S. Geological Survey Professional Paper. Vol. 1395. Washington, D.C.: U.S. Government Printing Office. doi: 10.3133/pp1395.
  2. ^ Tenzer, Róbert (2002). "Transformation of the Geodetic Horizontal Control to Another Reference Ellipsoid". Studia Geophysica et Geodaetica. 46 (1): 27–32. doi: 10.1023/A:1019881431482. S2CID  117114346. ProQuest  750849329.
  3. ^ For example, is called the second flattening in: Taff, Laurence G. (1980). An Astronomical Glossary (Technical report). MIT Lincoln Lab. p. 84.
    However, is called the second flattening in: Hooijberg, Maarten (1997). Practical Geodesy: Using Computers. Springer. p. 41. doi: 10.1007/978-3-642-60584-0_3.
  4. ^ Maling, Derek Hylton (1992). Coordinate Systems and Map Projections (2nd ed.). Oxford; New York: Pergamon Press. p. 65. ISBN  0-08-037233-3.
    Rapp, Richard H. (1991). Geometric Geodesy, Part I (Technical report). Ohio State Univ. Dept. of Geodetic Science and Surveying.
    Osborne, P. (2008). "The Mercator Projections" (PDF). §5.2. Archived from the original (PDF) on 2012-01-18.
  5. ^ Lapaine, Miljenko (2017). "Basics of Geodesy for Map Projections". In Lapaine, Miljenko; Usery, E. Lynn (eds.). Choosing a Map Projection. Lecture Notes in Geoinformation and Cartography. pp. 327–343. doi: 10.1007/978-3-319-51835-0_13. ISBN  978-3-319-51834-3.
    Karney, Charles F.F. (2023). "On auxiliary latitudes". Survey Review: 1–16. arXiv: 2212.05818. doi: 10.1080/00396265.2023.2217604. S2CID  254564050.
  6. ^ F. W. Bessel, 1825, Uber die Berechnung der geographischen Langen und Breiten aus geodatischen Vermessungen, Astron.Nachr., 4(86), 241–254, doi: 10.1002/asna.201011352, translated into English by C. F. F. Karney and R. E. Deakin as The calculation of longitude and latitude from geodesic measurements, Astron. Nachr. 331(8), 852–861 (2010), E-print arXiv: 0908.1824, Bibcode: 1825AN......4..241B