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    Empirical comparison between stochastic and deterministic modifiers over the French Auvergne geoid computation test-bed

    82610.pdf (1.448Mb)
    Access Status
    Open access
    Authors
    Goyal, Ropesh
    Ågren, J.
    Featherstone, Will
    Sjöberg, L.E.
    Dikshit, O.
    Balasubramanian, N.
    Date
    2021
    Type
    Journal Article
    
    Metadata
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    Citation
    Goyal, R. and Ågren, J. and Featherstone, W.E. and Sjöberg, L.E. and Dikshit, O. and Balasubramanian, N. 2021. Empirical comparison between stochastic and deterministic modifiers over the French Auvergne geoid computation test-bed. Survey Review.
    Source Title
    Survey Review
    DOI
    10.1080/00396265.2021.1871821
    ISSN
    0039-6265
    Faculty
    Faculty of Science and Engineering
    School
    School of Earth and Planetary Sciences (EPS)
    Remarks

    This is an accepted manuscript of an article published by Taylor & Francis in Survey Review on 17/01/2021 available online at http://www.tandfonline.com/10.1080/00396265.2021.1871821

    URI
    http://hdl.handle.net/20.500.11937/82548
    Collection
    • Curtin Research Publications
    Abstract

    © 2021 Survey Review Ltd. Since 2006, several different groups have computed geoid and/or quasigeoid (quasi/geoid) models for the Auvergne test area in central France using various approaches. In this contribution, we compute and compare quasigeoid models for Auvergne using Curtin University of Technology’s and the Swedish Royal Institute of Technology’s approaches. These approaches differ in many ways, such as their treatment of the input data, choice of type of spherical harmonic model (combined or satellite-only), form and sequence of correction terms applied, and different modified Stokes’s kernels (deterministic or stochastic). We have also compared our results with most of the previously reported studies over Auvergne in order to seek any improvements with respect to time [exceptions are when different subsets of data have been used]. All studies considered here compare the computed quasigeoid models with the same 75 GPS-levelling heights over Auvergne. The standard deviation for almost all of the computations (without any fitting) is of the order of 30–40 mm, so there is not yet any clear indication whether any approach is necessarily better than any other nor improving over time. We also recommend more standardisation on the presentation of quasi/geoid comparisons with GPS-levelling data so that results from different approaches over the same areas can be compared more objectively.

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