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Approximate decorrelation and non-isotropic smoothing of time-variable GRACE-type gravity field models

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Publication:1013508
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DOI10.1007/s00190-007-0143-3zbMath1158.86314OpenAlexW2160057192MaRDI QIDQ1013508

Jürgen Kusche

Publication date: 20 April 2009

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

Full work available at URL: https://doi.org/10.1007/s00190-007-0143-3


zbMATH Keywords

smoothingdecorrelationGRACEtime-variable gravity


Mathematics Subject Classification ID

Potentials, prospecting (86A20)


Related Items (1)

A first approach to learning a best basis for gravitational field modelling



Cites Work

  • Unnamed Item
  • Wavelet modeling of regional and temporal variations of the Earth's gravitational potential observed by GRACE
  • Regional gravity modeling in terms of spherical base functions
  • Accuracy assessment of the monthly GRACE geoids based upon a simulation
  • The determination of gravitational potential differences from satellite-to-satellite tracking
  • Nonstationary wavelets on the \(m\)-sphere for scattered data


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