Topography-Assisted downward Continuation of Airborne Gravity: An Application for Geoid Determination in Taiwan

We investigated the Fourier transform-based downward continuation (DWC) of airborne gravity anomalies around Taiwan assisted by topographic information. The topographic data are from the latest collections of elevations and ocean depths. The DWC employs a remove-compute-restore (RCR) procedure in wh...

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Main Author: Yu-Shen Hsiao Cheinway Hwang
Format: Article
Language:English
Published: Chinese Geoscience Union 2010-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v213p615.pdf
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spelling doaj-cc3b420082ca4ada9dc9a3955289564f2020-11-25T00:20:30ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802010-01-0121461510.3319/TAO.2009.07.09.01(T)938Topography-Assisted downward Continuation of Airborne Gravity: An Application for Geoid Determination in TaiwanYu-Shen Hsiao Cheinway HwangWe investigated the Fourier transform-based downward continuation (DWC) of airborne gravity anomalies around Taiwan assisted by topographic information. The topographic data are from the latest collections of elevations and ocean depths. The DWC employs a remove-compute-restore (RCR) procedure in which the topography is removed prior to computation and then restored to achieve stable solutions. The topographic gravity effect is evaluated point-wise using the Gaussian quadrature. A Gaussian filter with an optimal smoothing parameter reduces the noise-amplifying effect of DWC. Use of topography in DWC leads to improvements of 3 to 6 mgal of gravity on land. Surface and downward continued gravity anomalies are used to determine geoidal heights by least squares collocation (LSC) in a similar RCR procedure through the same topographic data. The accuracy of the geoidal heights at Taiwan¡¦s first-order leveling benchmarks is improved by 1 to 2 cm due to inclusion of downward continued airborne gravity. http://tao.cgu.org.tw/images/attachments/v213p615.pdf GeoidDownward continuationGravity anomalyLeast-squares collocationTopography
collection DOAJ
language English
format Article
sources DOAJ
author Yu-Shen Hsiao Cheinway Hwang
spellingShingle Yu-Shen Hsiao Cheinway Hwang
Topography-Assisted downward Continuation of Airborne Gravity: An Application for Geoid Determination in Taiwan
Terrestrial, Atmospheric and Oceanic Sciences
Geoid
Downward continuation
Gravity anomaly
Least-squares collocation
Topography
author_facet Yu-Shen Hsiao Cheinway Hwang
author_sort Yu-Shen Hsiao Cheinway Hwang
title Topography-Assisted downward Continuation of Airborne Gravity: An Application for Geoid Determination in Taiwan
title_short Topography-Assisted downward Continuation of Airborne Gravity: An Application for Geoid Determination in Taiwan
title_full Topography-Assisted downward Continuation of Airborne Gravity: An Application for Geoid Determination in Taiwan
title_fullStr Topography-Assisted downward Continuation of Airborne Gravity: An Application for Geoid Determination in Taiwan
title_full_unstemmed Topography-Assisted downward Continuation of Airborne Gravity: An Application for Geoid Determination in Taiwan
title_sort topography-assisted downward continuation of airborne gravity: an application for geoid determination in taiwan
publisher Chinese Geoscience Union
series Terrestrial, Atmospheric and Oceanic Sciences
issn 1017-0839
2311-7680
publishDate 2010-01-01
description We investigated the Fourier transform-based downward continuation (DWC) of airborne gravity anomalies around Taiwan assisted by topographic information. The topographic data are from the latest collections of elevations and ocean depths. The DWC employs a remove-compute-restore (RCR) procedure in which the topography is removed prior to computation and then restored to achieve stable solutions. The topographic gravity effect is evaluated point-wise using the Gaussian quadrature. A Gaussian filter with an optimal smoothing parameter reduces the noise-amplifying effect of DWC. Use of topography in DWC leads to improvements of 3 to 6 mgal of gravity on land. Surface and downward continued gravity anomalies are used to determine geoidal heights by least squares collocation (LSC) in a similar RCR procedure through the same topographic data. The accuracy of the geoidal heights at Taiwan¡¦s first-order leveling benchmarks is improved by 1 to 2 cm due to inclusion of downward continued airborne gravity.
topic Geoid
Downward continuation
Gravity anomaly
Least-squares collocation
Topography
url http://tao.cgu.org.tw/images/attachments/v213p615.pdf
work_keys_str_mv AT yushenhsiaocheinwayhwang topographyassisteddownwardcontinuationofairbornegravityanapplicationforgeoiddeterminationintaiwan
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