Effect of Qattara Depression on gravity and geoid using unclassified digital terrain models

The determination of the gravimetric geoid is based on the magnitude of the gravity observed at the topographic surface of the Earth. In order to satisfy Laplace’s equation, the masses between the surface of the Earth and the geoid must be removed or shifted inside the geoid. Then the gravity values...

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Bibliographic Details
Published in:Studia geophysica et geodaetica 2020-04, Vol.64 (2), p.186-201
Main Authors: Abd-Elmotaal, Hussein A., Kühtreiber, Norbert
Format: Article
Language:English
Subjects:
Atmospheric Sciences
Computation
Earth and Environmental Science
Earth Sciences
Earth surface
Geoid
Geoid determination
Geoids
Geologic depressions
Geophysics/Geodesy
Gravimetry
Gravitation
Gravity
Ocean models
Ocean stations
Prototypes
Reduction
Sea level
Structural Geology
Terrain models
Topography
Water masses
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Summary:The determination of the gravimetric geoid is based on the magnitude of the gravity observed at the topographic surface of the Earth. In order to satisfy Laplace’s equation, the masses between the surface of the Earth and the geoid must be removed or shifted inside the geoid. Then the gravity values have to be reduced to the geoid, forming the boundary values on the boundary surface. Gravity reduction techniques using unclassified Digital Terrain Models (DTM) usually presume that negative elevations are reserved for ocean stations. In case of Qattara Depression, the elevations are negative, i.e., below sea level. This leads to an obvious error in the topographic-isostatic reduction using, for example, TC-program employing unclassified DTM by assuming water masses filling the depression instead of air, besides computing at the non-existing sea level instead of computing at the actual negative topography. The aim of this paper is to determine the effect of Qattara Depression on gravity reduction and geoid computation, as a prototype of the effect of the unclassified land depressions on gravity reduction and geoid determination. The results show that the effect of Qattara Depression on the gravity reduction reaches 20 mGal and is restricted only to the depression area, while its effect on the geoid exceeds 1 m and has a regional effect which extends over a distance of about 1000 km.
ISSN:0039-3169
1573-1626
DOI:10.1007/s11200-018-1240-x