Regional Ground Surface Mass Variations Inversed by Radial Point-mass Model Method with Spatial Constraints

Radial point-mass model method is the disturbance gravity downward continuation in essence, which is an ill-posed problem. In general, the regularization method is an efficient way to get the reliable solution. To solve this problem, the radial point-mass model method is improved by using Helmert va...

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Main Authors: GUO Feixiao, SUN Zhongmiao, ZHAO Jun, MIAO Yuewang, XIAO Yun
Format: Article
Language:zho
Published: Surveying and Mapping Press 2018-05-01
Series:Acta Geodaetica et Cartographica Sinica
Subjects:
Online Access:http://html.rhhz.net/CHXB/html/2018-5-592.htm
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spelling doaj-2ad65979461449108e01fa7f784fb87b2020-11-24T22:53:40ZzhoSurveying and Mapping PressActa Geodaetica et Cartographica Sinica1001-15951001-15952018-05-0147559259910.11947/j.AGCS.2018.201705472018050547Regional Ground Surface Mass Variations Inversed by Radial Point-mass Model Method with Spatial ConstraintsGUO Feixiao0SUN Zhongmiao1ZHAO Jun2MIAO Yuewang3XIAO Yun4Information and Engineering University, Zhengzhou 450001, ChinaState Key Laboratory of Geo-information Engineering, Xi'an 710054, ChinaXi'an Technology Station of Surveying and Mapping, Xi'an 710054, ChinaXi'an Technology Station of Surveying and Mapping, Xi'an 710054, ChinaState Key Laboratory of Geo-information Engineering, Xi'an 710054, ChinaRadial point-mass model method is the disturbance gravity downward continuation in essence, which is an ill-posed problem. In general, the regularization method is an efficient way to get the reliable solution. To solve this problem, the radial point-mass model method is improved by using Helmert variance component estimation with adding spatial constraints from a practical point of view. Taking South America continent as study area, radial point-mass model method with spatial constraints is verified by experimental results. The experiments results show that the condition number of normal equations is decreasing obviously after adding spatial constraints. The inversion results of radial point-mass model method with spatial constraints are consistent with results of other methods. Furthermore, the radial point-mass model method with spatial constraints provides an alternative way to monitor regional surface mass variations by satellite gravimetry.http://html.rhhz.net/CHXB/html/2018-5-592.htmGRACE satellitetime-variable gravitypoint-mass modelspatial constraintsregularizationHelmert variance component estimation
collection DOAJ
language zho
format Article
sources DOAJ
author GUO Feixiao
SUN Zhongmiao
ZHAO Jun
MIAO Yuewang
XIAO Yun
spellingShingle GUO Feixiao
SUN Zhongmiao
ZHAO Jun
MIAO Yuewang
XIAO Yun
Regional Ground Surface Mass Variations Inversed by Radial Point-mass Model Method with Spatial Constraints
Acta Geodaetica et Cartographica Sinica
GRACE satellite
time-variable gravity
point-mass model
spatial constraints
regularization
Helmert variance component estimation
author_facet GUO Feixiao
SUN Zhongmiao
ZHAO Jun
MIAO Yuewang
XIAO Yun
author_sort GUO Feixiao
title Regional Ground Surface Mass Variations Inversed by Radial Point-mass Model Method with Spatial Constraints
title_short Regional Ground Surface Mass Variations Inversed by Radial Point-mass Model Method with Spatial Constraints
title_full Regional Ground Surface Mass Variations Inversed by Radial Point-mass Model Method with Spatial Constraints
title_fullStr Regional Ground Surface Mass Variations Inversed by Radial Point-mass Model Method with Spatial Constraints
title_full_unstemmed Regional Ground Surface Mass Variations Inversed by Radial Point-mass Model Method with Spatial Constraints
title_sort regional ground surface mass variations inversed by radial point-mass model method with spatial constraints
publisher Surveying and Mapping Press
series Acta Geodaetica et Cartographica Sinica
issn 1001-1595
1001-1595
publishDate 2018-05-01
description Radial point-mass model method is the disturbance gravity downward continuation in essence, which is an ill-posed problem. In general, the regularization method is an efficient way to get the reliable solution. To solve this problem, the radial point-mass model method is improved by using Helmert variance component estimation with adding spatial constraints from a practical point of view. Taking South America continent as study area, radial point-mass model method with spatial constraints is verified by experimental results. The experiments results show that the condition number of normal equations is decreasing obviously after adding spatial constraints. The inversion results of radial point-mass model method with spatial constraints are consistent with results of other methods. Furthermore, the radial point-mass model method with spatial constraints provides an alternative way to monitor regional surface mass variations by satellite gravimetry.
topic GRACE satellite
time-variable gravity
point-mass model
spatial constraints
regularization
Helmert variance component estimation
url http://html.rhhz.net/CHXB/html/2018-5-592.htm
work_keys_str_mv AT guofeixiao regionalgroundsurfacemassvariationsinversedbyradialpointmassmodelmethodwithspatialconstraints
AT sunzhongmiao regionalgroundsurfacemassvariationsinversedbyradialpointmassmodelmethodwithspatialconstraints
AT zhaojun regionalgroundsurfacemassvariationsinversedbyradialpointmassmodelmethodwithspatialconstraints
AT miaoyuewang regionalgroundsurfacemassvariationsinversedbyradialpointmassmodelmethodwithspatialconstraints
AT xiaoyun regionalgroundsurfacemassvariationsinversedbyradialpointmassmodelmethodwithspatialconstraints
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