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Methods and Technologies for Measuring the Earth’s Gravity Field Parameters

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  • © 2022

Overview

  • Provides extensive information on methods for terrestrial gravimetry
  • Describes data processing methods for onboard gravity anomaly measurements
  • Guides to the development of earth's gravity field models

Part of the book series: Earth Systems Data and Models (ESDM, volume 5)

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Table of contents (6 chapters)

Keywords

About this book

This book offers extensive information on the operation of gravimeters, including airborne, marine and terrestrial ones, and on the associated data processing methods such as optimal and adaptive filtering, smoothing, structural and parametric identification. Further, it describes specific features relating to the study of the gravitational field in remote areas of the Earth, with the necessary modifications of equipment and software for all-latitude applications. Findings from gravity studies in such remote areas are also presented. Advanced methods for studying the gravitational field, including those for simultaneous determination of gravity anomalies and deflection of the vertical are described and analyzed in detail. Gravity gradiometers and cold atom gravimeters are also covered. Last but not least, the book deals with the development of Earth’s gravity field models and their various applications, including map-aided navigation, with a special attention to model accuracy estimation. Gathering research findings and best practice recommendations relating to Earth’s gravity field measurements, collected by a team of researchers and professionals, the book offers a unique guide for engineers, scientists and graduate students dealing with terrestrial, marine and airborne gravimetry.  It will also help other specialists involved in developing and using navigation systems in practice, including designers of gravimetric equipment and navigators.

Editors and Affiliations

  • Concern CSRI Elektropribor,ITMO University, St. Petersburg, Russia

    V. G. Peshekhonov, O. A. Stepanov

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