On the topographic bias by harmonic continuation of the geopotential for a spherical sea-level approximation

Topography is a problem in geoid determination by the Stokes formula, a high degree Earth Gravitational Model (EGM), or for a combination thereof. Herein, we consider this problem in analytical/harmonic downward continuation of the external potential at point P to a geocentric spherical sea level ap...

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Main Author: Sjöberg Lars E.
Format: Article
Language:English
Published: De Gruyter 2024-11-01
Series:Journal of Geodetic Science
Subjects:
Online Access:https://doi.org/10.1515/jogs-2022-0180
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author Sjöberg Lars E.
author_facet Sjöberg Lars E.
author_sort Sjöberg Lars E.
collection DOAJ
description Topography is a problem in geoid determination by the Stokes formula, a high degree Earth Gravitational Model (EGM), or for a combination thereof. Herein, we consider this problem in analytical/harmonic downward continuation of the external potential at point P to a geocentric spherical sea level approximation in geoid determination as well as to a sphere through the footpoint at the topography of the normal through P. Decomposing the topographic bias into a Bouguer shell component and a terrain component, we derive these components. It is shown that there is no terrain bias outside a spherical dome of base radius equal to the height H P of P above the sphere, and the height of the dome is about 0.4 × H P. In the case of dealing with an EGM, utilizing Molodensky truncation coefficients is one way to cope with the bias.
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spelling doaj-art-3fc070c8fbb348b68033f4b024794f302025-08-20T02:23:36ZengDe GruyterJournal of Geodetic Science2081-99432024-11-011411124410.1515/jogs-2022-0180On the topographic bias by harmonic continuation of the geopotential for a spherical sea-level approximationSjöberg Lars E.0Geodesy and Geoinformatics, Royal Institute of Technology: Kungliga Tekniska Hogskolan, Stockholm, SwedenTopography is a problem in geoid determination by the Stokes formula, a high degree Earth Gravitational Model (EGM), or for a combination thereof. Herein, we consider this problem in analytical/harmonic downward continuation of the external potential at point P to a geocentric spherical sea level approximation in geoid determination as well as to a sphere through the footpoint at the topography of the normal through P. Decomposing the topographic bias into a Bouguer shell component and a terrain component, we derive these components. It is shown that there is no terrain bias outside a spherical dome of base radius equal to the height H P of P above the sphere, and the height of the dome is about 0.4 × H P. In the case of dealing with an EGM, utilizing Molodensky truncation coefficients is one way to cope with the bias.https://doi.org/10.1515/jogs-2022-0180analytical continuationdownward continuationharmonic continuation(quasi)geoid determinationtopographic bias
spellingShingle Sjöberg Lars E.
On the topographic bias by harmonic continuation of the geopotential for a spherical sea-level approximation
Journal of Geodetic Science
analytical continuation
downward continuation
harmonic continuation
(quasi)geoid determination
topographic bias
title On the topographic bias by harmonic continuation of the geopotential for a spherical sea-level approximation
title_full On the topographic bias by harmonic continuation of the geopotential for a spherical sea-level approximation
title_fullStr On the topographic bias by harmonic continuation of the geopotential for a spherical sea-level approximation
title_full_unstemmed On the topographic bias by harmonic continuation of the geopotential for a spherical sea-level approximation
title_short On the topographic bias by harmonic continuation of the geopotential for a spherical sea-level approximation
title_sort on the topographic bias by harmonic continuation of the geopotential for a spherical sea level approximation
topic analytical continuation
downward continuation
harmonic continuation
(quasi)geoid determination
topographic bias
url https://doi.org/10.1515/jogs-2022-0180
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