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    Is Australian data really validating EGM2008, or is EGM2008 just in/validating Australia data?

    13368.pdf (2.940Mb)
    Access Status
    Open access
    Authors
    Claessens, Sten
    Featherstone, Will
    Anjasmara, Ira
    Filmer, Michael
    Date
    2009
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Claessens, S.J. and Featherstone, W.E. and Anjasmara, I.M. and Filmer, M.S. 2009. Is Australian data really validating EGM2008, or is EGM2008 just in/validating Australia data? Newton's Bulletin. 4: pp. 207-251.
    Source Title
    Newton's Bulletin
    Additional URLs
    http://www.iges.polimi.it/Newton/Newton_4/Report_AAA1_Australia.pdf
    ISSN
    18108555
    School
    Department of Spatial Sciences
    Remarks

    Published by International Geoid Service (IGeS)

    URI
    http://hdl.handle.net/20.500.11937/31388
    Collection
    • Curtin Research Publications
    Abstract

    The tide-free release of the EGM2008 combined global geopotential model and its tide-free pre-release PGM2007A are compared with Australian land, marine and airborne gravity observations, co-located GPS-levelling on the [admittedly problematic] Australian Height Datum, astrogeodetic deflections of the vertical, and the AUSGeoid98 regional gravimetric quasigeoid model. In all comparisons, EGM2008 performs better than any previous global gravity model. The standard deviation of the differences between free-air gravity anomalies from EGM2008 and free-air gravity anomalies from Australian land gravity observations is 5.5 mGal, compared to, e.g., 11.7 mGal for EGM96. Furthermore, the standard deviation of the differences between height anomalies from EGM2008 and anation-wide set of 254 GPS-levelling points is 17.3 cm, compared to, e.g., 33.4 cmfor EGM96. In the comparisons with GPS-levelling, EGM2008 also outperforms AUSGeoid98 (standard deviation of 19.1 cm in the differences with the nation-wide set of 254 GPS-levelling points), and the same holds for the comparison to astrogeodetic deflections of the vertical. However, due to the poor quality of some of the Australian data, we cannot legitimately claim to truly validate EGM2008. Instead, EGM2008 confirms the already-known problems with the Australian data, as well as revealing some previously unknown problems. If one wants to claim validation, then EGM2008 is validated implicitly because it can confirm the errors in our regional data. Simply, EGM2008 is a good model over Australia.

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