Investigation of crustal motion in Europe by analysing the European VLBI sessions

Since 1990 the International VLBI Service for Geodesy and Astrometry (IVS) has been performing geodetic Very Long Baseline Interferometry (VLBI) observations within the European geodetic VLBI network. In this work, 114 European VLBI sessions from January 1990 to September 2011 are analysed using the...

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Published in:Acta Geodaetica et Geophysica
Main Authors: Krásná, H., Tierno Ros, C., Pavetich, P., Böhm, J., Nilsson, T., Schuh, H.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2013
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Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_321315
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_321315 2023-05-15T16:41:19+02:00 Investigation of crustal motion in Europe by analysing the European VLBI sessions Krásná, H. Tierno Ros, C. Pavetich, P. Böhm, J. Nilsson, T. Schuh, H. 2013 https://gfzpublic.gfz-potsdam.de/pubman/item/item_321315 unknown info:eu-repo/semantics/altIdentifier/doi/10.1007/s40328-013-0034-4 https://gfzpublic.gfz-potsdam.de/pubman/item/item_321315 Acta Geodaetica et Geophysica info:eu-repo/semantics/article 2013 ftgfzpotsdam https://doi.org/10.1007/s40328-013-0034-4 2022-09-14T05:54:42Z Since 1990 the International VLBI Service for Geodesy and Astrometry (IVS) has been performing geodetic Very Long Baseline Interferometry (VLBI) observations within the European geodetic VLBI network. In this work, 114 European VLBI sessions from January 1990 to September 2011 are analysed using the Vienna VLBI Software (VieVS). A total of 58 baselines with lengths ranging from 59 m to 4581 km are investigated and the lengths of most of them indicate repeatabilities at the sub-centimetre level. The horizontal station motions which describe the motion of the Eurasian plate are compared to the NUVEL-1A and MORVEL tectonic plate models. Intraplate crustal motions are investigated by estimating the station velocities with respect to Wettzell (Germany), a station on the geodynamically stable part of Eurasia. The northern part of Europe is dominated by the postglacial isostatic rebound, confirmed by four VLBI sites in this region with an uplift from 2.89±0.71 mm/yr (Svetloe, Russia) to 7.23±1.00 mm/yr (Ny-Ålesund, Norway) with respect to the central part of the European plate. Besides the vertical uplift, these radio telescopes evidence a horizontal motion from the centre of the former ice sheet towards its border. In the southern part of Europe the motion of the VLBI sites is caused by the collision of the African plate with the Eurasian plate, while the stations on the stable part of Europe do not present any significant relative motions. Our results are compared against those by Haas et al. (J. Geodyn. 35:391–414, 2003) and with velocities of the current reference frame of the International Global Navigation Satellite Systems Service. Article in Journal/Newspaper Ice Sheet Ny Ålesund Ny-Ålesund GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Norway Ny-Ålesund Acta Geodaetica et Geophysica 48 4 389 404
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language unknown
description Since 1990 the International VLBI Service for Geodesy and Astrometry (IVS) has been performing geodetic Very Long Baseline Interferometry (VLBI) observations within the European geodetic VLBI network. In this work, 114 European VLBI sessions from January 1990 to September 2011 are analysed using the Vienna VLBI Software (VieVS). A total of 58 baselines with lengths ranging from 59 m to 4581 km are investigated and the lengths of most of them indicate repeatabilities at the sub-centimetre level. The horizontal station motions which describe the motion of the Eurasian plate are compared to the NUVEL-1A and MORVEL tectonic plate models. Intraplate crustal motions are investigated by estimating the station velocities with respect to Wettzell (Germany), a station on the geodynamically stable part of Eurasia. The northern part of Europe is dominated by the postglacial isostatic rebound, confirmed by four VLBI sites in this region with an uplift from 2.89±0.71 mm/yr (Svetloe, Russia) to 7.23±1.00 mm/yr (Ny-Ålesund, Norway) with respect to the central part of the European plate. Besides the vertical uplift, these radio telescopes evidence a horizontal motion from the centre of the former ice sheet towards its border. In the southern part of Europe the motion of the VLBI sites is caused by the collision of the African plate with the Eurasian plate, while the stations on the stable part of Europe do not present any significant relative motions. Our results are compared against those by Haas et al. (J. Geodyn. 35:391–414, 2003) and with velocities of the current reference frame of the International Global Navigation Satellite Systems Service.
format Article in Journal/Newspaper
author Krásná, H.
Tierno Ros, C.
Pavetich, P.
Böhm, J.
Nilsson, T.
Schuh, H.
spellingShingle Krásná, H.
Tierno Ros, C.
Pavetich, P.
Böhm, J.
Nilsson, T.
Schuh, H.
Investigation of crustal motion in Europe by analysing the European VLBI sessions
author_facet Krásná, H.
Tierno Ros, C.
Pavetich, P.
Böhm, J.
Nilsson, T.
Schuh, H.
author_sort Krásná, H.
title Investigation of crustal motion in Europe by analysing the European VLBI sessions
title_short Investigation of crustal motion in Europe by analysing the European VLBI sessions
title_full Investigation of crustal motion in Europe by analysing the European VLBI sessions
title_fullStr Investigation of crustal motion in Europe by analysing the European VLBI sessions
title_full_unstemmed Investigation of crustal motion in Europe by analysing the European VLBI sessions
title_sort investigation of crustal motion in europe by analysing the european vlbi sessions
publishDate 2013
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_321315
geographic Norway
Ny-Ålesund
geographic_facet Norway
Ny-Ålesund
genre Ice Sheet
Ny Ålesund
Ny-Ålesund
genre_facet Ice Sheet
Ny Ålesund
Ny-Ålesund
op_source Acta Geodaetica et Geophysica
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s40328-013-0034-4
https://gfzpublic.gfz-potsdam.de/pubman/item/item_321315
op_doi https://doi.org/10.1007/s40328-013-0034-4
container_title Acta Geodaetica et Geophysica
container_volume 48
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