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Curtin University of Technology

GEODETIC AND ENVIRONMENTAL APPLICATION OF SATELLITE ALTIMETRY OVER LAND

Investigators
  • Professor Will Featherstone
  • Professor Philippa Berry, De Montfort University, England
  • Ms Xiaoli Deng
  • Mr Richard Hilton, De Montfort University, England

    Funding Sources

  • Australian Research Council, International Researcher Exchange Scheme
  • Curtin University Postgraduate Scholarship
  • International Postgraduate Research Scholarship

    Status

  • Started 1999, ongoing

    Summary
    A new technique, devised at De Montfort University, uses satellite-borne radar altimeters to determine terrain heights and soil-surface moisture on land. This collaborative program between Curtin and De Montfort Universities is using these independent satellite altimeter data to correct errors in Australian digital elevation models, to quantify the effects of these errors on the determination of the Australian gravity field, and to generate calibrated time-series of soil-surface moisture over the Australian continent. The results give accuracy estimates to the increasing number of users of digital elevation models, an improved determination of the Australian geoid, and create a totally new data set for the environmental sciences.

    Results
    Satellite altimeter-derived heights from ERS-1 have been compared with heights defined by six digital elevation models (DEM) over Ausstralia. These comparisons show that there are systematic differences between the altimeter-derived heights and the DEM defined heights. The agreements with the Australian DEM (which uses more reliable data than the other two models) are sightly better. Asssuming the altimeter data and Australian DEM are accurate, this indicates that the global DEMs should not be relied upon too greatly in this part of the world.

    Figure 1. Differences between altimeter-derived heights and JGP95E DEM heights in northern Queensland

    In Figure 1, there are may areas with geographically correlated differences. It is thought that this is due to the JGP95E DEM being derived from gravity observation elevations. These elevations do not accurately sample the topographic shape. Typically the JGP95E DEM heights are underestimated in high-land regions and over-estimated in low-land regions. This is due to the logisitics of collecting gravity data with helecopters. Also in Figure 1, there is a north-south line aparent in the differences. This is due to the JGP95E model mbeign construicted from Australian data in the west and NIMA data in the east.

    References
    Hilton, R.D., W.E. Featherstone, P.A.M. Berry, C.P.D Johnston and J.F. Kirby (2002) Comparison of Digital Elevation Models (DEMs) over Australia and external validation using ERS-1 satellite radar altimetry, Australian Journal of Earth Sciences (submitted). PDF preprint
    Berry, P A M, Thornton, S R and Featherstone, W E (1998) Accuracy assessment of altimeter-derived orthometric heights using regional digital elevation models, paper presented to European Geophysical Society General Meeting, Vienna, Austria, April.
    Berry, P A M, Thornton, S R and Featherstone, W E (1998) Validation of altimeter-derived orthometric heights over Australia, paper presented to British Group of Altimeter Specialists Conference, Liverpool, England, April.
    Berry P A M, Sanders R F, Leenmans C, Bron E (1998) Generating orthometric heights from the ERS-1 altimeter geodetic mission dataset: results from an expert systems approach, in: Forsberg R, Feissl M, Deitrich R (eds) Geodesy on the Move, Springer, Berlin, Germany, 113-118.
    Berry P A M, Bron E, Sanders R F, Leenmans C (1998) Use of ERS-1 land altimetry to validate the GLOBE global digital elevation model, in: Forsberg R, Feissl M, Deitrich R (eds) Geodesy on the Move, Springer, Berlin, Germany, 119-124.

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