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A Determination of the Earth's Gravity Field in Spheroidal Coordinates

The earth's gravity field G * at a point P in the region surrounding the earth's surface is defined as the force acting on a unit mass concentrated at P. This is a force resulting from two components: (1) G1 due to the gravitational attraction of the earth's mass, and (2) G2 due to the earth's rotation.

Identiferoai:union.ndltd.org:UTAHS/oai:digitalcommons.usu.edu:etd-7849
Date01 May 1961
CreatorsHamilton, M. Spencer, Jr.
PublisherDigitalCommons@USU
Source SetsUtah State University
Detected LanguageEnglish
Typetext
Formatapplication/pdf
SourceAll Graduate Theses and Dissertations
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