The Earth's gravity field from the STEP mission

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  • Technical University of Munich (TUM)
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Original languageEnglish
Pages (from-to)A113-A117
JournalClassical and quantum gravity
Volume13
Issue number11A
Publication statusPublished - 1 Nov 1996
Externally publishedYes

Abstract

The geodesy experiment on STEP aims at the precise and detailed determination of the spatial variations of the Earth's gravitational field by measuring the cross-track gradient along the orbit. If the envisaged gradiometer precision of 10-4 E Hz-1/2 can be reached and all other potential error sources, such as alignment, pointing and time-varying eigengravitation can be kept below this limit, a spatial resolution of about 100 km half-wavelength will be attained with a cumulative geoid error of below 2 cm (except in the polar areas).

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The Earth's gravity field from the STEP mission. / Sneeuw, N.; Rummel, R.; Müller, J.
In: Classical and quantum gravity, Vol. 13, No. 11A, 01.11.1996, p. A113-A117.

Research output: Contribution to journalArticleResearchpeer review

Sneeuw N, Rummel R, Müller J. The Earth's gravity field from the STEP mission. Classical and quantum gravity. 1996 Nov 1;13(11A):A113-A117. doi: 10.1088/0264-9381/13/11A/015
Sneeuw, N. ; Rummel, R. ; Müller, J. / The Earth's gravity field from the STEP mission. In: Classical and quantum gravity. 1996 ; Vol. 13, No. 11A. pp. A113-A117.
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