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Topographic and atmospheric corrections of gravimetric geoid determination with special emphasis on the effects of harmonics of degrees zero and one
Authors:L E Sjöberg
Institution:(1) Department of Geodesy and Photogrammetry, Royal Institute of Technology, SE-100 44 Stockholm, Sweden e-mail: sjoberg@geomatics.kth.se; Tel.: +46-8-790-73-30; Fax: +46-8-7907343, SE
Abstract: The topographic and atmospheric effects of gravimetric geoid determination by the modified Stokes formula, which combines terrestrial gravity and a global geopotential model, are presented. Special emphasis is given to the zero- and first-degree effects. The normal potential is defined in the traditional way, such that the disturbing potential in the exterior of the masses contains no zero- and first-degree harmonics. In contrast, it is shown that, as a result of the topographic masses, the gravimetric geoid includes such harmonics of the order of several centimetres. In addition, the atmosphere contributes with a zero-degree harmonic of magnitude within 1 cm. Received: 5 November 1999 / Accepted: 22 January 2001
Keywords::   Atmospheric Effects –  Geoid –  Topographic Effects
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