Performance of three types of Stokes's kernel in the combined solution for the geoid

When regional gravity data are used to compute a gravimetric geoid in conjunction with a geopotential model, it is sometimes implied that the terrestrial gravity data correct any erroneous wavelengths present in the geopotential model. This assertion is investigated. The propagation of errors from t...

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Main Authors: Vanicek, P., Featherstone, Will
Format: Journal Article
Published: Springer-Verlag 1998
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/28888
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author Vanicek, P.
Featherstone, Will
author_facet Vanicek, P.
Featherstone, Will
author_sort Vanicek, P.
building Curtin Institutional Repository
collection Online Access
description When regional gravity data are used to compute a gravimetric geoid in conjunction with a geopotential model, it is sometimes implied that the terrestrial gravity data correct any erroneous wavelengths present in the geopotential model. This assertion is investigated. The propagation of errors from the low-frequency terrestrial gravity field into the geoid is derived for the spherical Stokes integral, the spheroidal Stokes integral and the Molodensky-modified spheroidal Stokes integral. It is shown that error-free terrestrial gravity data, if used in a spherical cap of limited extent, cannot completely correct the geopotential model. Using a standard norm, it is shown that the spheroidal and Molodensky-modified integration kernels offer a preferable approach. This is because they can filter out a large amount of the low-frequency errors expected to exist in terrestrial gravity anomalies and thus rely more on the low-frequency geopotential model, which currently offers the best source of this information.
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spelling curtin-20.500.11937-288882017-09-13T15:16:05Z Performance of three types of Stokes's kernel in the combined solution for the geoid Vanicek, P. Featherstone, Will Geoid determination - Modified kernels - Error propagation - High-pass filtering When regional gravity data are used to compute a gravimetric geoid in conjunction with a geopotential model, it is sometimes implied that the terrestrial gravity data correct any erroneous wavelengths present in the geopotential model. This assertion is investigated. The propagation of errors from the low-frequency terrestrial gravity field into the geoid is derived for the spherical Stokes integral, the spheroidal Stokes integral and the Molodensky-modified spheroidal Stokes integral. It is shown that error-free terrestrial gravity data, if used in a spherical cap of limited extent, cannot completely correct the geopotential model. Using a standard norm, it is shown that the spheroidal and Molodensky-modified integration kernels offer a preferable approach. This is because they can filter out a large amount of the low-frequency errors expected to exist in terrestrial gravity anomalies and thus rely more on the low-frequency geopotential model, which currently offers the best source of this information. 1998 Journal Article http://hdl.handle.net/20.500.11937/28888 10.1007/s001900050209 Springer-Verlag restricted
spellingShingle Geoid determination - Modified kernels - Error propagation - High-pass filtering
Vanicek, P.
Featherstone, Will
Performance of three types of Stokes's kernel in the combined solution for the geoid
title Performance of three types of Stokes's kernel in the combined solution for the geoid
title_full Performance of three types of Stokes's kernel in the combined solution for the geoid
title_fullStr Performance of three types of Stokes's kernel in the combined solution for the geoid
title_full_unstemmed Performance of three types of Stokes's kernel in the combined solution for the geoid
title_short Performance of three types of Stokes's kernel in the combined solution for the geoid
title_sort performance of three types of stokes's kernel in the combined solution for the geoid
topic Geoid determination - Modified kernels - Error propagation - High-pass filtering
url http://hdl.handle.net/20.500.11937/28888