On the use of airborne gravimetry in gravity field modelling: Experiences from the AGMASCO project

Citation
L. Bastos et al., On the use of airborne gravimetry in gravity field modelling: Experiences from the AGMASCO project, PHYS CH P A, 25(1), 2000, pp. 1-7
Citations number
15
Categorie Soggetti
Earth Sciences
Journal title
PHYSICS AND CHEMISTRY OF THE EARTH PART A-SOLID EARTH AND GEODESY
ISSN journal
14641895 → ACNP
Volume
25
Issue
1
Year of publication
2000
Pages
1 - 7
Database
ISI
SICI code
1464-1895(2000)25:1<1:OTUOAG>2.0.ZU;2-1
Abstract
Important areas of the earth are still not covered by accurate gravity meas urements. The gravity field may be determined by using different techniques but airborne gravity surveying is becoming the most powerful tool availabl e today. One of the main problems in airborne gravity is the separation of the verti cal accelerations acting on the airborne platform from the natural gravity signal. With the advances in DGPS techniques new prospects arise for gravit y field recovery which are of great importance for geodesy, geophysics ocea nography and satellite navigation. Furthermore, airborne gravimetric measur ements depend not only on the determination of the position but also on the attitude of the aircraft. Inertial systems can provide attitude as well as information on short-term accelerations, which are more problematic for th e gravimeter. A proper integration of these systems may allow a further imp rovement of the whole technique where the quality of both the accelerometer s and the gyros is the key sensing element. In the scope of the MAST III Pr oject AGMASCO, an airborne geoid mapping system was successfully implemente d in different aeroplanes. The characteristics of the aeroplane and the fli ght parameters play a major role in airborne measurements. Within AGMASCO the airborne system was applied both in a close and an open ocean (Skagerrak, Fram Strait and Azores) areas. The system proved to be a powerful tool in a variety of conditions. The results obtained showed that an accuracy better than 2mGal over 5 to 6 kilometres can be achieved. This was proven by comparison of the airborne data with ground truth and sa tellite data. This accuracy makes the system interesting for use in various applications including geophysical exploitation. Different hardware installations were experienced and the methods validated . Recovery of the gravity values directly from measurements with the Lacost e & Romberg air/sea gravimeter and from measurements with the inertial sens ors was analysed. The potential of these sensors to recover gravity and the experience gained within this project are reported here. (C) 2000 Elsevier Science Ltd. All rights reserved.