GPS coordinate transformations and their use in gravimetry

Geodetic coordinates on Australian maps are referenced to the Australian Geodectic Datum 1984 (AGD84). Topographic elevations are referred to the Australian Height Datum (AHD). Conversely, GPS yields 3-D Cartesian coordinates and coordinate differences in the World Geodetic System 1984 (WGS84). The...

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Bibliographic Details
Main Author: Featherstone, Will
Format: Journal Article
Published: CSIRO Publishing 1993
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/5937
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author Featherstone, Will
author_facet Featherstone, Will
author_sort Featherstone, Will
building Curtin Institutional Repository
collection Online Access
description Geodetic coordinates on Australian maps are referenced to the Australian Geodectic Datum 1984 (AGD84). Topographic elevations are referred to the Australian Height Datum (AHD). Conversely, GPS yields 3-D Cartesian coordinates and coordinate differences in the World Geodetic System 1984 (WGS84). The difference between coordinates of the same point on the Earth's surface varies between 150 m to 200 m over continental Australia. This study presents a method of transforming between GPS (WGS84) and AGD84 latitude, longitude and AHD. This permits GPS-aided gravity data to be integrated with other geophysical data referred to the AGD84. A new rigorous formula to simultaneously determine the latitude, free-air and slab Bouguer corrections from GPS and geoid information is derived. It is demonstrated that, if an incorrect elevation datum is used for gravimetric data reduction, a different gravity anomaly is produced.
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spelling curtin-20.500.11937-59372017-09-13T16:02:18Z GPS coordinate transformations and their use in gravimetry Featherstone, Will coordinate transformations gravimetry GPS Geodetic coordinates on Australian maps are referenced to the Australian Geodectic Datum 1984 (AGD84). Topographic elevations are referred to the Australian Height Datum (AHD). Conversely, GPS yields 3-D Cartesian coordinates and coordinate differences in the World Geodetic System 1984 (WGS84). The difference between coordinates of the same point on the Earth's surface varies between 150 m to 200 m over continental Australia. This study presents a method of transforming between GPS (WGS84) and AGD84 latitude, longitude and AHD. This permits GPS-aided gravity data to be integrated with other geophysical data referred to the AGD84. A new rigorous formula to simultaneously determine the latitude, free-air and slab Bouguer corrections from GPS and geoid information is derived. It is demonstrated that, if an incorrect elevation datum is used for gravimetric data reduction, a different gravity anomaly is produced. 1993 Journal Article http://hdl.handle.net/20.500.11937/5937 10.1071/EG993487 CSIRO Publishing restricted
spellingShingle coordinate transformations
gravimetry
GPS
Featherstone, Will
GPS coordinate transformations and their use in gravimetry
title GPS coordinate transformations and their use in gravimetry
title_full GPS coordinate transformations and their use in gravimetry
title_fullStr GPS coordinate transformations and their use in gravimetry
title_full_unstemmed GPS coordinate transformations and their use in gravimetry
title_short GPS coordinate transformations and their use in gravimetry
title_sort gps coordinate transformations and their use in gravimetry
topic coordinate transformations
gravimetry
GPS
url http://hdl.handle.net/20.500.11937/5937