Elipticitet

Izvor: Wikipedia

Elipticitet ili spljoštenost obrtnog sferoida predstavlja meru pomeranja pola prema ekvatoru.[1][2][3][4][5]

{}_{\color{white}x}f=\mbox{ver}(o\!\varepsilon)=2\sin^2\left(\frac{o\!\varepsilon}{2}\right)=1-\cos(o\!\varepsilon)=\frac{a-b}{a};\,\!
f'=\tan^2\left(\frac{o\!\varepsilon}{2}\right)=\frac{1-\cos(o\!\varepsilon)}{1+\cos(o\!\varepsilon)}=\frac{a-b}{a+b}.\,\!

Reflist[uredi - уреди]

  1. Maling, Derek Hylton (1992). Coordinate Systems and Map Projections (2nd izd.). Oxford; New York: Pergamon Press. ISBN 0-08-037233-3. 
  2. Snyder, John P. (1987). Map Projections: A Working Manual. U.S. Geological Survey Professional Paper. 1395. Washington, D.C.: United States Government Printing Office. http://pubs.er.usgs.gov/pubs/pp/pp1395. 
  3. Torge, W. (2001). Geodesy (3rd edition). de Gruyter. ISBN 3-11-017072-8
  4. Osborne, P. (2008). The Mercator Projections Chapter 5.
  5. Rapp, Richard H. (1991). Geometric Geodesy, Part I. Dept. of Geodetic Science and Surveying, Ohio State Univ., Columbus, Ohio. [1]