High-Resolution Grids of Gravimetric Terrain Correction and Complete Bouguer Corrections Over Australia

Complete Bouguer corrections have been computed over the Australian mainland and Tasmania on a 9 arc-second grid (~250 m spatial resolution) from version 2 of the GEODATA digital elevation model (DEM) of Australia. These include the Bouguer plate correction to the geoid (mean sea level) and the plan...

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Main Authors: Kirby, Jon, Featherstone, Will
Format: Journal Article
Published: CSIRO Publishing 2002
Subjects:
Online Access:http://www.publish.csiro.au/nid/225/issue/4497.htm
http://hdl.handle.net/20.500.11937/40149
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author Kirby, Jon
Featherstone, Will
author_facet Kirby, Jon
Featherstone, Will
author_sort Kirby, Jon
building Curtin Institutional Repository
collection Online Access
description Complete Bouguer corrections have been computed over the Australian mainland and Tasmania on a 9 arc-second grid (~250 m spatial resolution) from version 2 of the GEODATA digital elevation model (DEM) of Australia. These include the Bouguer plate correction to the geoid (mean sea level) and the planar terrain correction residual to this plate out to a radius of 50 km (beyond Hammer zone M). A constant topographic density of 2670 kg.m-3 has been used for both correction terms. The terrain corrections were computed using a planar two-dimensional fast Fourier transform (FFT) algorithm.
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spelling curtin-20.500.11937-401492017-01-30T14:40:06Z High-Resolution Grids of Gravimetric Terrain Correction and Complete Bouguer Corrections Over Australia Kirby, Jon Featherstone, Will digital elevation model (DEM) Bouguer correction gravity anomaly Australia terrain correction fast Fourier transform (FFT) Complete Bouguer corrections have been computed over the Australian mainland and Tasmania on a 9 arc-second grid (~250 m spatial resolution) from version 2 of the GEODATA digital elevation model (DEM) of Australia. These include the Bouguer plate correction to the geoid (mean sea level) and the planar terrain correction residual to this plate out to a radius of 50 km (beyond Hammer zone M). A constant topographic density of 2670 kg.m-3 has been used for both correction terms. The terrain corrections were computed using a planar two-dimensional fast Fourier transform (FFT) algorithm. 2002 Journal Article http://hdl.handle.net/20.500.11937/40149 http://www.publish.csiro.au/nid/225/issue/4497.htm CSIRO Publishing fulltext
spellingShingle digital elevation model (DEM)
Bouguer correction
gravity anomaly
Australia
terrain correction
fast Fourier transform (FFT)
Kirby, Jon
Featherstone, Will
High-Resolution Grids of Gravimetric Terrain Correction and Complete Bouguer Corrections Over Australia
title High-Resolution Grids of Gravimetric Terrain Correction and Complete Bouguer Corrections Over Australia
title_full High-Resolution Grids of Gravimetric Terrain Correction and Complete Bouguer Corrections Over Australia
title_fullStr High-Resolution Grids of Gravimetric Terrain Correction and Complete Bouguer Corrections Over Australia
title_full_unstemmed High-Resolution Grids of Gravimetric Terrain Correction and Complete Bouguer Corrections Over Australia
title_short High-Resolution Grids of Gravimetric Terrain Correction and Complete Bouguer Corrections Over Australia
title_sort high-resolution grids of gravimetric terrain correction and complete bouguer corrections over australia
topic digital elevation model (DEM)
Bouguer correction
gravity anomaly
Australia
terrain correction
fast Fourier transform (FFT)
url http://www.publish.csiro.au/nid/225/issue/4497.htm
http://hdl.handle.net/20.500.11937/40149