Open Access

Downloads

Download data is not yet available.

Abstract

The normal gravity potential is easily determined by satellites, but it has no relation with some classical normal gravity formulae, such as Cassini’s or Helmert’s formulae, which are using in some countries. This paper presents a formula for determining the normal gravity potential and it’s parameters from a classical normal gravity formula with given flatenning α and angular velocity  of the Earth. Parameters fM and equatorial radius R are to be determined. The normal potential is used for establishing the anomaly of gravity potential (perturbating potential), which is necessary for determining the deflections of the vertical, the heights of the geoid by Bruns' formula, instead of using gravity anomaly in. Stokes’ formula or Stokes’ exspansion. In the next paper, we shall present the application of our formula for determining the geoid heights.



Author's Affiliation
Article Details

Issue: Vol 6 No 1&2 (2003)
Page No.: 45-49
Published: Feb 28, 2003
Section: Article
DOI: https://doi.org/10.32508/stdj.v6i1&2.3304

 Copyright Info

Creative Commons License

Copyright: The Authors. This is an open access article distributed under the terms of the Creative Commons Attribution License CC-BY 4.0., which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

 How to Cite
Huu Nghia, H., & Van Nhac, T. (2003). DETERMINATION OF THE NORMAL GRAVITY POTENTIAL FROM A NORMAL GRAVITY FORMULA FOR ESTABLISHING THE ANOMALY OF POTENTIAL. Science and Technology Development Journal, 6(1&2), 45-49. https://doi.org/https://doi.org/10.32508/stdj.v6i1&2.3304

 Cited by



Article level Metrics by Paperbuzz/Impactstory
Article level Metrics by Altmetrics

 Article Statistics
HTML = 674 times
Download PDF   = 307 times
Total   = 307 times