Refinement of Gravimetric Geoid Using GPS and Levelling Data

A gravimetric geoid model does not allow the accurate transformation of Global Positioning System (GPS) ellipsoidal heights to Australian Height Datum (AHD) heights in the Perth region of Western Australia. This is predominantly due to the effect of the geological structures associated with the Dar...

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Main Author: Featherstone, Will
Format: Journal Article
Published: American Society of Civil Engineers 2000
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/34505
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author Featherstone, Will
author_facet Featherstone, Will
author_sort Featherstone, Will
building Curtin Institutional Repository
collection Online Access
description A gravimetric geoid model does not allow the accurate transformation of Global Positioning System (GPS) ellipsoidal heights to Australian Height Datum (AHD) heights in the Perth region of Western Australia. This is predominantly due to the effect of the geological structures associated with the Darling Fault, the availability and quality of data, and the possibility of distortions in the AHD. Therefore, a combined solution is sought, where 99 co-located GPS and AHD heights are used to adjust the gravimetric geoid such that it provides a model of the separation between the AHD and the GRS80 reference ellipsoid. This data combination was investigated using least squares collocation and continuous curvature splines in tension. The least squares collocation technique was found to give an improved model of the AHD-GRS80 separation, as shown by a standard deviation of fit of the combined model to the control data of ±8 mm. In comparison, the gravimetric geoid gives a standard deviation of fit to the control data of ±128 mm.
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spelling curtin-20.500.11937-345052017-09-13T15:55:36Z Refinement of Gravimetric Geoid Using GPS and Levelling Data Featherstone, Will Gravity Least squares collocation Height Splines Australia GPS Geoid A gravimetric geoid model does not allow the accurate transformation of Global Positioning System (GPS) ellipsoidal heights to Australian Height Datum (AHD) heights in the Perth region of Western Australia. This is predominantly due to the effect of the geological structures associated with the Darling Fault, the availability and quality of data, and the possibility of distortions in the AHD. Therefore, a combined solution is sought, where 99 co-located GPS and AHD heights are used to adjust the gravimetric geoid such that it provides a model of the separation between the AHD and the GRS80 reference ellipsoid. This data combination was investigated using least squares collocation and continuous curvature splines in tension. The least squares collocation technique was found to give an improved model of the AHD-GRS80 separation, as shown by a standard deviation of fit of the combined model to the control data of ±8 mm. In comparison, the gravimetric geoid gives a standard deviation of fit to the control data of ±128 mm. 2000 Journal Article http://hdl.handle.net/20.500.11937/34505 10.1061/(ASCE)0733-9453(2000)126:2(27) American Society of Civil Engineers fulltext
spellingShingle Gravity
Least squares collocation
Height
Splines
Australia
GPS
Geoid
Featherstone, Will
Refinement of Gravimetric Geoid Using GPS and Levelling Data
title Refinement of Gravimetric Geoid Using GPS and Levelling Data
title_full Refinement of Gravimetric Geoid Using GPS and Levelling Data
title_fullStr Refinement of Gravimetric Geoid Using GPS and Levelling Data
title_full_unstemmed Refinement of Gravimetric Geoid Using GPS and Levelling Data
title_short Refinement of Gravimetric Geoid Using GPS and Levelling Data
title_sort refinement of gravimetric geoid using gps and levelling data
topic Gravity
Least squares collocation
Height
Splines
Australia
GPS
Geoid
url http://hdl.handle.net/20.500.11937/34505