The (first) flattening
of a spheroid, also called oblateness or ellipticity,
is defined as
 |
(1)
|
where
is the polar radius
and
is the equatorial radius.
It is related to the eccentricity
by
(Snyder 1987, p. 13).
A so-called second and third flattening may be defined as
 |
(4)
|
and
 |
(5)
|
(Karney).
See also
Oblate Spheroid,
Prolate
Spheroid,
Spheroid
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References
Karney, C. F. F. "On Auxiliary latitudes." 21 May 2023. https://arxiv.org/abs/2212.05818.Snyder,
J. P. Map
Projections--A Working Manual. U. S. Geological Survey Professional
Paper 1395. Washington, DC: U. S. Government Printing Office, 1987.Referenced
on Wolfram|Alpha
Flattening
Cite this as:
Weisstein, Eric W. "Flattening." From
MathWorld--A Wolfram Web Resource. https://mathworld.wolfram.com/Flattening.html
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