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Computing components of the gravity field induced by distant topographic masses and condensed masses over the entire Earth using the 1-D FFT approach

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Publication:1601239
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DOI10.1007/S00190-001-0227-4zbMath1007.86002OpenAlexW2001224960MaRDI QIDQ1601239

R. Smith

Publication date: 19 June 2002

Published in: Journal of Geodesy (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1007/s00190-001-0227-4


zbMATH Keywords

attractiongravitational potentialone-dimensional fast Fourier transformStokes-Helmert scheme


Mathematics Subject Classification ID

Computational methods for problems pertaining to geophysics (86-08) Geodesy, mapping problems (86A30)


Related Items (2)

A comparison of the tesseroid, prism and point-mass approaches for mass reductions in gravity field modelling ⋮ The topographic bias by analytical continuation in physical geodesy







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