Equal Area Blocks for the Representation of the Global Mean Gravity Anomaly Field
Author | : Dhaneshwar P. Hajela |
Publisher | : |
Total Pages | : 54 |
Release | : 1975 |
Genre | : Gravity anomalies |
ISBN | : |
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Author | : Dhaneshwar P. Hajela |
Publisher | : |
Total Pages | : 54 |
Release | : 1975 |
Genre | : Gravity anomalies |
ISBN | : |
Author | : Athanasios Dermanis |
Publisher | : |
Total Pages | : 636 |
Release | : 1974 |
Genre | : Aeronautics in geodesy |
ISBN | : |
Author | : Athanasios Dermanis |
Publisher | : |
Total Pages | : 642 |
Release | : 1976 |
Genre | : Earth (Planet) |
ISBN | : |
Author | : Hans Sünkel |
Publisher | : |
Total Pages | : 484 |
Release | : 1978 |
Genre | : Approximation theory |
ISBN | : |
Author | : Luman E. Wilcox |
Publisher | : |
Total Pages | : 318 |
Release | : 1974 |
Genre | : Gravity |
ISBN | : |
Mean gravity anomaly values which represent 1 degree x 1 degree surface areas can be predicted on the continents by geophysical gravity correlation methods whether or nor measured gravity data exists within those 1 degree x 1 degree areas. These methods take into consideration the earth's structure, composition, and response to changes in surficial mass distribution by means of observed or computed correlations between gravity and other geophysical parameters within geologic/tectonic provinces. Linear basic prediction functions, used to describe and predict the relationships between gravity and elevation, are shown to be a natural consequence of the properties of gravity reduction procedures and the observed behavior of gravity anomalies within structurally homogeneous regions. (Modified author abstract).
Author | : Fernando Sansò |
Publisher | : Springer Science & Business Media |
Total Pages | : 748 |
Release | : 2013-02-13 |
Genre | : Science |
ISBN | : 3540747001 |
This book will be based on the material of the lecture noties in several International Schools for the Determination and Use of the Geoid, organized by the International Geoid Serivice of the International Association of Geodesy. It consolidates, unifies, and streamlines this material in a unique way not covereed by the few other books that exist on this subjext. More specifically, the book presents (for the first time in a single volume) the theory and methodology of the most common technique used for precise determination of the geoid, including the computation of the marine geoid from satellite altimetry data. These are illustrated by specific examples and actual computations of local geoids. In addition, the book provides the fundamentals of estimating orthometric heights without spirit levelling, by properly combining a geoid with heights from GPS. Besides the geodectic and geophysical uses, this last application has made geoid computation methods very popular in recent years because the entire GPS and GIS user communities are interested in estimating geoid undulations in order to convert GPS heights to physically meaningful orthometric heights (elevations above mean sea level). The overall purpose of the book is, therefore, to provide the user community (academics, graduate students, geophysicists, engineers, oceanographers, GIS and GPS users, researchers) with a self-contained textbook, which will supply them with the complete roadmap of estimating geoid undulations, from the theoretical definitions and formulas to the available numerical methods and their implementation and the test in practice.
Author | : Peiliang Xu |
Publisher | : Springer Science & Business Media |
Total Pages | : 375 |
Release | : 2008-02-27 |
Genre | : Science |
ISBN | : 354074584X |
This volume of proceedings is a collection of refereed papers resulting from the VI Hotine-Marussi Symposium on Theoretical and Computational Geodesy. The papers cover almost every topic of geodesy, including satellite gravity modeling, geodynamics, GPS data processing, statistical estimation and prediction theory, and geodetic inverse problem theory. In addition, particular attention is paid to topics of fundamental importance in the next one or two decades in Earth Science.