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Title of Journal: J Geod

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Abbravation: Journal of Geodesy

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Springer Berlin Heidelberg

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DOI

10.1007/s00190-015-0813-5

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1432-1394

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Alternative validation method of satellite gradiom

Authors: Michal Šprlák Eliška Hamáčková Pavel Novák
Publish Date: 2015/04/24
Volume: 89, Issue: 8, Pages: 757-773
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Abstract

Integral transforms of the disturbing gravitational potential derived from satellite altimetry onto satellite gradiometric data are formulated investigated and applied in this article First corresponding differential operators that relate the disturbing gravitational potential to the six components of the disturbing gradiometric tensor in the spherical local northoriented frame are applied to the spherical AbelPoisson integral equation This yields six new integral equations for which respective kernel functions are given in both spectral and spatial forms Second truncation error formulas for each of the integral transforms are provided in the spectral form Also expressions for the corresponding truncation error coefficients are derived Third practical estimators for evaluation of the disturbing gravitational gradients are formulated and their correctness and expected accuracy are investigated Finally the practical estimators are applied for validation of a sample of the gradiometric data provided by the GOCE satellite mission Obtained results demonstrate applicability of the new apparatus as an alternative validation method of the satellite gravitational gradientsMichal Šprlák and Pavel Novák were supported by the project no GA1508045S of the Czech Science Foundation Eliška Hamáčková was supported by the project SGS2013024 The authors thank P L Woodworth for providing the mean dynamic topography models Thoughtful and constructive comments of three anonymous reviewers are gratefully acknowledged Thanks are also extended to the EditorinChief R Klees and the responsible editor C Jekeli for handling our manuscriptProposition 8 follows from Eqs 40–42 and from the spectral form of the modified isotropic kernel Kbullet given by Eq 37 Note that Eq 52 defines the socalled Paul coefficients which can be evaluated by recurrence formulas see eg Paul 1973To prove Proposition 9 we start with the modified truncation error coefficient Q nbullet First the spatial form of the modified isotropic kernel Kbullet see Eq 37 is inserted into Eq 40 Second we make use of the analytical solution for the resulting integral given by Pavlis 1991 Eq A 29a–b and Eq 53 immediately follow The modified truncation error coefficients Q nbullet t and Q nbullet tt are the first and second derivatives of Q nbullet with respect to the variable t see Eqs 41 42 Performing the differentiations of Eq 53 we get the recurrence formulas of Eqs 54 and 55


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Other Papers In This Journal:

  1. Spherical integral formulas for upward/downward continuation of gravitational gradients onto gravitational gradients
  2. New versions of the BDS/GNSS zenith tropospheric delay model IGGtrop
  3. Alternative validation method of satellite gradiometric data by integral transform of satellite altimetry data
  4. Earth’s gravity field modelling based on satellite accelerations derived from onboard GPS phase measurements
  5. Separation of global time-variable gravity signals into maximally independent components
  6. The effect on the geoid of lateral topographic density variations
  7. Atmospheric and oceanic forcing of the rapid polar motion
  8. Methodology and use of tensor invariants for satellite gravity gradiometry
  9. Precise orbit determination for the FORMOSAT-3/COSMIC satellite mission using GPS
  10. Local Multiscale Modelling of Geoid Undulations from Deflections of the Vertical
  11. An absolute calibration site for radar altimeters in the continental domain: Lake Issykkul in Central Asia
  12. Thermosteric Effects on Interannual and Long-term Global Mean Sea Level Changes
  13. Application of SWACI products as ionospheric correction for single-point positioning: a comparative study
  14. Statistical modeling for the mitigation of GPS multipath delays from day-to-day range measurements
  15. On the double-peak spectrum of the Chandler wobble
  16. Basic equations for constructing geopotential models from the gravitational potential derivatives of the first and second orders in the terrestrial reference frame
  17. Bias in GRACE estimates of ice mass change due to accompanying sea-level change
  18. A new isostatic model of the lithosphere and gravity field
  19. Convex optimization under inequality constraints in rank-deficient systems
  20. On the deformation analysis of point fields

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