Geoid

E Geoid ass e phsyesche Modell vun der Form vun der Äerd. E representéiert d'Form, déi d'Uewerfläch vun den Ozeaner géif unhuele wa se nëmmen der Gravitat…

Geoid
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Äerdmagnéitfeld, Ofwäichunge staark iwwerhéicht

E Geoid ass e phsyesche Modell vun der Form vun der Äerd. E representéiert d'Form, déi d'Uewerfläch vun den Ozeaner géif unhuele wa se nëmmen der Gravitatioun an der Rotatioun vun der Äerd ausgesat wier an et keng aner Aflëss wéi de Wand oder d'Gezäite géife ginn.[1]

Kuckt och

Literatur

  • Christoph Reigber, Peter Schwintzer: Das Schwerefeld der Erde. Physik in unserer Zeit 34(5), S. 206–212 (2003), ISSN 0031-9252.
  • Erwin Groten: Geodesy and the Earth’s Gravity Field – Vol.I Principles and Conventional methods. Bonn 1979.
  • Intergovermental Committee On Surveying & Mapping: Geocentric Datum of Australia – Technical Manual, Version 2.2. PDF, Stand: 2005.
  • Wolfgang Torge: Geodäsie. 2. Auflage. Walter de Gruyter, Berlin u.a. 2003, ISBN 3-11-017545-2

Um Spaweck

Referenzen

  1. ↑ quora.com: If you were to measure gravity on the surface of the ocean over the deepest place in the world would it be 9.81 ms/s2? Or would water have less gravitational pull than a mass of rock. Äntwert vum Frank Heile, P.h.D. Physics, den 19. Abrëll 2013


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