Abstract

Australian quasigeoid modelling: Review, current status and future plans

Highlights

  • Experimental quasigeoid models and “patching”2.1 Patching an error in Port Phillip Bay, Victoria, SE Australia Following the release of the AUSGeoid2020 model, a number of independent tests – using GDA2020 ellipsoidal heights and levelling data that were not included in AUSGeoid2020 – were conducted by State Government departments to ensure the model was precise and “fit for purpose”

  • Geocentric Datum of Australia 2020 ellipsoidal heights in a more direct manner without the need for post-surveying adjustments

  • We have provided a historical review of regional geoid and quasigeoid modelling over the Australian continent

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Summary

Experimental quasigeoid models and “patching”

2.1 Patching an error in Port Phillip Bay, Victoria, SE Australia Following the release of the AUSGeoid2020 model, a number of independent tests – using GDA2020 ellipsoidal heights and levelling data that were not included in AUSGeoid2020 – were conducted by State Government departments to ensure the model was precise and “fit for purpose”. Fig 2.3.1 (a) Standard deviations (m) of gravimetric quasigeoid models for parameter sweeps of the FEO kernel modification degree and spherical integration cap radius versus GNSS-levelling data after removal of a tilted plane using the G1 term (solid lines) and the planar terrain correction (dashed lines—from Featherstone et al 2018a), both determined from 1”×1”grids. (b) Standard deviations (m) of gravimetric quasigeoid models for parameter sweeps of FEO kernel modification degree and spherical integration cap radius versus GNSS-levelling data after removal of a tilted plane using the G1 term (solid lines) and the planar terrain corrections, both determined from 1’×1’ grids.

Potential improvements to be offered by airborne gravimetry data
Findings
Concluding remarks
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