Astrogeodetic Validation of Gravimetric Quasigeoid Models in the German Alps - First Results

In regions with a rough topography, e.g. the European Alps, the accuracy of geoid or quasigeoid models is often reduced. For the validation and accuracy assessment of gravimetric models, astronomical levelling is a well-suited independent method. In a test area, located in the German Alps, a new ast...

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Main Authors: Hirt, Christian, Denker, H., Flury, J., Lindau, A., Seeber, G.
Other Authors: Assoc.Prof.Dr.Ali KILIOGLU
Format: Conference Paper
Published: Harita Dergisi 2009
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/40111
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author Hirt, Christian
Denker, H.
Flury, J.
Lindau, A.
Seeber, G.
author2 Assoc.Prof.Dr.Ali KILIOGLU
author_facet Assoc.Prof.Dr.Ali KILIOGLU
Hirt, Christian
Denker, H.
Flury, J.
Lindau, A.
Seeber, G.
author_sort Hirt, Christian
building Curtin Institutional Repository
collection Online Access
description In regions with a rough topography, e.g. the European Alps, the accuracy of geoid or quasigeoid models is often reduced. For the validation and accuracy assessment of gravimetric models, astronomical levelling is a well-suited independent method. In a test area, located in the German Alps, a new astrogeodetic data set was acquired using the Hannover Digital Zenith Camera System. Vertical deflections were determined at 100 new stations (spacing about 230 m) arranged in a profile of 23 km length. Repeated observations at 38 stations in different nights reveal an observational accuracy of about 0.08. In order to precisely interpolate the vertical deflection data between adjacent stations, topographic reductions of the observed deflections are carried out using a high-resolution digital terrain model.A least squares prediction approach is applied for the interpolation of a dense profile of deflection data. Eventually, the topography effect is restored. By computing the normal correction, the deflection data is reduced to the quasigeoid domain. The accuracy of the computed astrogeodetic quasigeoid profile is estimated to be at the millimeter-level. The available quasigeoid models, namely the German Combined Geoid GCG2005, the Digital Finite Height Reference Surface DFHRS and the quasigeoid by IAPG (TU Munich), are in agreement with the high-precision astrogeodetic quasigeoid profile by about 8 mm, 20 mm and 4 mm (RMS), respectively. A comparison of the astrogeodetic profile with GPS/levelling data yielded residuals of 10 mm.
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institution Curtin University Malaysia
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last_indexed 2025-11-14T09:01:41Z
publishDate 2009
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spelling curtin-20.500.11937-401112022-12-09T07:12:33Z Astrogeodetic Validation of Gravimetric Quasigeoid Models in the German Alps - First Results Hirt, Christian Denker, H. Flury, J. Lindau, A. Seeber, G. Assoc.Prof.Dr.Ali KILIOGLU Prof.Dr.Rene FORSBERG astrogeodetic quasigeoid profile Digital Zenith Camera System vertical - deflection local - quasigeoid evaluation In regions with a rough topography, e.g. the European Alps, the accuracy of geoid or quasigeoid models is often reduced. For the validation and accuracy assessment of gravimetric models, astronomical levelling is a well-suited independent method. In a test area, located in the German Alps, a new astrogeodetic data set was acquired using the Hannover Digital Zenith Camera System. Vertical deflections were determined at 100 new stations (spacing about 230 m) arranged in a profile of 23 km length. Repeated observations at 38 stations in different nights reveal an observational accuracy of about 0.08. In order to precisely interpolate the vertical deflection data between adjacent stations, topographic reductions of the observed deflections are carried out using a high-resolution digital terrain model.A least squares prediction approach is applied for the interpolation of a dense profile of deflection data. Eventually, the topography effect is restored. By computing the normal correction, the deflection data is reduced to the quasigeoid domain. The accuracy of the computed astrogeodetic quasigeoid profile is estimated to be at the millimeter-level. The available quasigeoid models, namely the German Combined Geoid GCG2005, the Digital Finite Height Reference Surface DFHRS and the quasigeoid by IAPG (TU Munich), are in agreement with the high-precision astrogeodetic quasigeoid profile by about 8 mm, 20 mm and 4 mm (RMS), respectively. A comparison of the astrogeodetic profile with GPS/levelling data yielded residuals of 10 mm. 2009 Conference Paper http://hdl.handle.net/20.500.11937/40111 Harita Dergisi restricted
spellingShingle astrogeodetic quasigeoid profile
Digital Zenith Camera System
vertical - deflection
local - quasigeoid evaluation
Hirt, Christian
Denker, H.
Flury, J.
Lindau, A.
Seeber, G.
Astrogeodetic Validation of Gravimetric Quasigeoid Models in the German Alps - First Results
title Astrogeodetic Validation of Gravimetric Quasigeoid Models in the German Alps - First Results
title_full Astrogeodetic Validation of Gravimetric Quasigeoid Models in the German Alps - First Results
title_fullStr Astrogeodetic Validation of Gravimetric Quasigeoid Models in the German Alps - First Results
title_full_unstemmed Astrogeodetic Validation of Gravimetric Quasigeoid Models in the German Alps - First Results
title_short Astrogeodetic Validation of Gravimetric Quasigeoid Models in the German Alps - First Results
title_sort astrogeodetic validation of gravimetric quasigeoid models in the german alps - first results
topic astrogeodetic quasigeoid profile
Digital Zenith Camera System
vertical - deflection
local - quasigeoid evaluation
url http://hdl.handle.net/20.500.11937/40111