Comparison of numerical solution strategies for gravity field recovery from GOCE SGG observations implemented on a parallel platform

The recovery of a full set of gravity field parameters from satellite gravity gradiometry (SGG) is a huge numerical and computational task. In practice, parallel computing has to be applied to estimate the more than 90 000 harmonic coefficients parameterizing the Earth’s gravity field up to a maximu...

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Main Authors: R. Pail, G. Plank
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/1/39/2003/adgeo-1-39-2003.pdf
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spelling doaj-e427a25735694323a8c31988cedfdb672020-11-24T21:51:12ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592003-01-0113945Comparison of numerical solution strategies for gravity field recovery from GOCE SGG observations implemented on a parallel platformR. PailG. PlankThe recovery of a full set of gravity field parameters from satellite gravity gradiometry (SGG) is a huge numerical and computational task. In practice, parallel computing has to be applied to estimate the more than 90 000 harmonic coefficients parameterizing the Earth’s gravity field up to a maximum spherical harmonic degree of 300. Three independent solution strategies, i.e. two iterative methods (preconditioned conjugate gradient method, semi-analytic approach) and a strict solver (Distributed Non-approximative Adjustment), which are operational on a parallel platform (‘Graz Beowulf Cluster’), are assessed and compared both theoretically and on the basis of a realistic-as-possible numerical simulation, regarding the accuracy of the results, as well as the computational effort. Special concern is given to the correct treatment of the coloured noise characteristics of the gradiometer. The numerical simulations show that there are no significant discrepancies among the solutions of the three methods. The newly proposed Distributed Nonapproximative Adjustment approach, which is the only one of the three methods that solves the inverse problem in a strict sense, also turns out to be a feasible method for practical applications.<br><br><b>Key words.</b> Spherical harmonics – satellite gravity gradiometry – GOCE – parallel computing – Beowulf clusterhttp://www.adv-geosci.net/1/39/2003/adgeo-1-39-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. Pail
G. Plank
spellingShingle R. Pail
G. Plank
Comparison of numerical solution strategies for gravity field recovery from GOCE SGG observations implemented on a parallel platform
Advances in Geosciences
author_facet R. Pail
G. Plank
author_sort R. Pail
title Comparison of numerical solution strategies for gravity field recovery from GOCE SGG observations implemented on a parallel platform
title_short Comparison of numerical solution strategies for gravity field recovery from GOCE SGG observations implemented on a parallel platform
title_full Comparison of numerical solution strategies for gravity field recovery from GOCE SGG observations implemented on a parallel platform
title_fullStr Comparison of numerical solution strategies for gravity field recovery from GOCE SGG observations implemented on a parallel platform
title_full_unstemmed Comparison of numerical solution strategies for gravity field recovery from GOCE SGG observations implemented on a parallel platform
title_sort comparison of numerical solution strategies for gravity field recovery from goce sgg observations implemented on a parallel platform
publisher Copernicus Publications
series Advances in Geosciences
issn 1680-7340
1680-7359
publishDate 2003-01-01
description The recovery of a full set of gravity field parameters from satellite gravity gradiometry (SGG) is a huge numerical and computational task. In practice, parallel computing has to be applied to estimate the more than 90 000 harmonic coefficients parameterizing the Earth’s gravity field up to a maximum spherical harmonic degree of 300. Three independent solution strategies, i.e. two iterative methods (preconditioned conjugate gradient method, semi-analytic approach) and a strict solver (Distributed Non-approximative Adjustment), which are operational on a parallel platform (‘Graz Beowulf Cluster’), are assessed and compared both theoretically and on the basis of a realistic-as-possible numerical simulation, regarding the accuracy of the results, as well as the computational effort. Special concern is given to the correct treatment of the coloured noise characteristics of the gradiometer. The numerical simulations show that there are no significant discrepancies among the solutions of the three methods. The newly proposed Distributed Nonapproximative Adjustment approach, which is the only one of the three methods that solves the inverse problem in a strict sense, also turns out to be a feasible method for practical applications.<br><br><b>Key words.</b> Spherical harmonics – satellite gravity gradiometry – GOCE – parallel computing – Beowulf cluster
url http://www.adv-geosci.net/1/39/2003/adgeo-1-39-2003.pdf
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