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Geoid Modeling.pdf

5_cazenave.pdf

🔗 Source: web.archive.org

📊 Size: 750 KB

👤 Author: MDUNCAN

⬇️ Downloads: 308

Summary

The gravitational potential at point P outside the Earth due to the heterogeneous mass distribution inside the Earth volume is expressed through a spherical harmonic expansion, with Stokes' coefficients representing integral functions of the mass distribution. The geoid is the equipotential surface of the gravity potential, coinciding with the mean sea level, and its height is measured above a reference ellipsoid. Gravity anomalies and deflection of the vertical are related to the perturbing potential, and the power spectrum of the geopotential is given by the degree variance of the geopotential coefficients. The GEM-T3 geopotential model provides coefficients up to degree 50, and the long-wavelength geoid surface is presented, as well as the medium and short-wavelength geoid undulations mapped by the Geosat satellite.

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Description

The gravitational potential at point P outside the Earth due to the heterogeneous mass distribution inside the Earth volume is expressed through a spherical...

Technical Information

File Format: PDF
File Size: 750 KB
Pages: 8
Language: EN
Author: MDUNCAN
Total Downloads: 308
Last Updated: 1 week ago

Document Overview

This PDF document about Geoid Modeling provides comprehensive information and guidance. Whether you're a beginner or advanced user, this resource offers valuable insights into Geoid Modeling.