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1000 Titel
  • An Improved Model of the Earth’s Static Gravity Field Solely Derived from Reprocessed GOCE Data
1000 Autor/in
  1. Brockmann, Jan Martin |
  2. Schubert, Till |
  3. Schuh, Wolf-Dieter |
1000 Erscheinungsjahr 2021
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2021-01-18
1000 Erschienen in
1000 Quellenangabe
  • 42(2):277-316
1000 Copyrightjahr
  • 2021
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s10712-020-09626-0 |
1000 Publikationsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:title>Abstract</jats:title><jats:p>After it was found that the gravity gradients observed by the Gravity field and steady-state Ocean Circulation Explorer (GOCE) satellite could be significantly improved by an advanced calibration, a reprocessing project for the entire mission data set was initiated by ESA and performed by the GOCE High-level processing facility (GOCE HPF). One part of the activity was delivering the gravity field solutions, where the improved level 1b and level 2 data serve as an input for global gravity field recovery. One well-established approach for the analysis of GOCE observations is the so-called time-wise approach. Basic characteristics of the GOCE time-wise solutions is that only GOCE observations are included to remain independent of any other gravity field observables and that emphasis is put on the stochastic modeling of the observations’ uncertainties. As a consequence, the time-wise solutions provide a GOCE-only model and a realistic uncertainty description of the model in terms of the full covariance matrix of the model coefficients. Within this contribution, we review the GOCE time-wise approach and discuss the impact of the improved data and modeling applied in the computation of the new GO_CONS_EGM_TIM_RL06 solution. The model reflects the Earth’s static gravity field as observed by the GOCE satellite during its operation. As nearly all global gravity field models, it is represented as a spherical harmonic expansion, with maximum degree 300. The characteristics of the model and the contributing data are presented, and the internal consistency is demonstrated. The updated solution nicely meets the official GOCE mission requirements with a global mean accuracy of about 2 cm in terms of geoid height and 0.6 mGal in terms of gravity anomalies at ESA’s target spatial resolution of 100 km. Compared to its RL05 predecessor, three kinds of improvements are shown, i.e., (1) the mean global accuracy increases by 10–25%, (2) a more realistic uncertainty description and (3) a local reduction of systematic errors in the order of centimeters.</jats:p>
1000 Sacherschließung
lokal Gravity gradients
lokal Uncertainty description
lokal Article
lokal Spherical harmonics
lokal GOCE
lokal Stochastic modeling
lokal Time-wise approach
lokal Global gravity field model
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0002-7647-4515|https://frl.publisso.de/adhoc/uri/U2NodWJlcnQsIFRpbGw=|https://frl.publisso.de/adhoc/uri/U2NodWgsIFdvbGYtRGlldGVy
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1000 Erstellt am 2023-04-27T15:01:16.699+0200
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1000 Zuletzt bearbeitet 2023-10-20T14:22:50.596+0200
1000 Objekt bearb. Fri Oct 20 14:22:50 CEST 2023
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