BIFROST project: 3-D crustal deformation rates derived from GPS confirm postglacial rebound in Fennoscandia

Since autumn 1993 the BIFROST project has provided daily GPS solutions of geodetic positions from a network of more than 40 stations covering, a large area of the Baltic shield. This area is expected to show large vertical motion due to glacial isostatic rebound following the deglaciation at the end...

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Published in:Earth, Planets and Space
Main Authors: Scherneck, Hans-Georg, Johansson, Jan M., Vermeer, Martin, Davis, James L., Milne, Glenn A., Mitrovica, Jerry
Format: Article in Journal/Newspaper
Language:English
Published: SpringerOpen 2001
Subjects:
Online Access:http://nrs.harvard.edu/urn-3:HUL.InstRepos:41401437
https://doi.org/10.1186/BF03352398
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spelling ftharvardudash:oai:dash.harvard.edu:1/41401437 2023-05-15T16:12:05+02:00 BIFROST project: 3-D crustal deformation rates derived from GPS confirm postglacial rebound in Fennoscandia Scherneck, Hans-Georg Johansson, Jan M. Vermeer, Martin Davis, James L. Milne, Glenn A. Mitrovica, Jerry 2001 application/pdf http://nrs.harvard.edu/urn-3:HUL.InstRepos:41401437 https://doi.org/10.1186/BF03352398 en_US eng SpringerOpen Earth, Planets and Space Scherneck, Hans-Georg, Jan M. Johansson, Martin Vermeer, James L. Davis, Glenn A. Milne, and Jerry X. Mitrovica. 2001. “BIFROST Project: 3-D Crustal Deformation Rates Derived from GPS Confirm Postglacial Rebound in Fennoscandia.” Earth, Planets and Space 53 (7): 703–8. https://doi.org/10.1186/bf03352398. 1343-8832 1880-5981 http://nrs.harvard.edu/urn-3:HUL.InstRepos:41401437 doi:10.1186/BF03352398 Journal Article 2001 ftharvardudash https://doi.org/10.1186/BF03352398 https://doi.org/10.1186/bf03352398 2022-04-04T11:36:11Z Since autumn 1993 the BIFROST project has provided daily GPS solutions of geodetic positions from a network of more than 40 stations covering, a large area of the Baltic shield. This area is expected to show large vertical motion due to glacial isostatic rebound following the deglaciation at the end of the Pleistocene. This paper will discuss the inference of three-dimensional rates of crustal motion at the GPS stations with respect to (1) a plate-fixed average for the horizontal components; (2) a geocentric reference in order to infer absolute changes of sea level from vertical crustal motion and models of geoidal rebound. We show that the horizontal strain rate pattern is largely dominated by unilateral extension and not exhibiting horizontal shear to an important extent. In regard to the vertical motion a crucial issue is the stability of the geocentre in the GPS frame. We show results from an Empirical Orthogonal Function analysis that attenuates regionally correlated noise. In all components our observations suggest reasonably close agreement with forward computions on the basis of postglacial isostatic adjustment. A dominant tectonic signal would lead to a certain fraction of the batch of baselines to exhibit shortening. A tectonic process leading to a similar pattern of horizontal motion as expected from postglacial rebound can safely be dismissed in the context of the currently accepted plate tectonic setting. Thus, our baseline rate comparison will be a critical first order test of the prevailing style of deformation. Version of Record Article in Journal/Newspaper Fennoscandia Harvard University: DASH - Digital Access to Scholarship at Harvard Earth, Planets and Space 53 7 703 708
institution Open Polar
collection Harvard University: DASH - Digital Access to Scholarship at Harvard
op_collection_id ftharvardudash
language English
description Since autumn 1993 the BIFROST project has provided daily GPS solutions of geodetic positions from a network of more than 40 stations covering, a large area of the Baltic shield. This area is expected to show large vertical motion due to glacial isostatic rebound following the deglaciation at the end of the Pleistocene. This paper will discuss the inference of three-dimensional rates of crustal motion at the GPS stations with respect to (1) a plate-fixed average for the horizontal components; (2) a geocentric reference in order to infer absolute changes of sea level from vertical crustal motion and models of geoidal rebound. We show that the horizontal strain rate pattern is largely dominated by unilateral extension and not exhibiting horizontal shear to an important extent. In regard to the vertical motion a crucial issue is the stability of the geocentre in the GPS frame. We show results from an Empirical Orthogonal Function analysis that attenuates regionally correlated noise. In all components our observations suggest reasonably close agreement with forward computions on the basis of postglacial isostatic adjustment. A dominant tectonic signal would lead to a certain fraction of the batch of baselines to exhibit shortening. A tectonic process leading to a similar pattern of horizontal motion as expected from postglacial rebound can safely be dismissed in the context of the currently accepted plate tectonic setting. Thus, our baseline rate comparison will be a critical first order test of the prevailing style of deformation. Version of Record
format Article in Journal/Newspaper
author Scherneck, Hans-Georg
Johansson, Jan M.
Vermeer, Martin
Davis, James L.
Milne, Glenn A.
Mitrovica, Jerry
spellingShingle Scherneck, Hans-Georg
Johansson, Jan M.
Vermeer, Martin
Davis, James L.
Milne, Glenn A.
Mitrovica, Jerry
BIFROST project: 3-D crustal deformation rates derived from GPS confirm postglacial rebound in Fennoscandia
author_facet Scherneck, Hans-Georg
Johansson, Jan M.
Vermeer, Martin
Davis, James L.
Milne, Glenn A.
Mitrovica, Jerry
author_sort Scherneck, Hans-Georg
title BIFROST project: 3-D crustal deformation rates derived from GPS confirm postglacial rebound in Fennoscandia
title_short BIFROST project: 3-D crustal deformation rates derived from GPS confirm postglacial rebound in Fennoscandia
title_full BIFROST project: 3-D crustal deformation rates derived from GPS confirm postglacial rebound in Fennoscandia
title_fullStr BIFROST project: 3-D crustal deformation rates derived from GPS confirm postglacial rebound in Fennoscandia
title_full_unstemmed BIFROST project: 3-D crustal deformation rates derived from GPS confirm postglacial rebound in Fennoscandia
title_sort bifrost project: 3-d crustal deformation rates derived from gps confirm postglacial rebound in fennoscandia
publisher SpringerOpen
publishDate 2001
url http://nrs.harvard.edu/urn-3:HUL.InstRepos:41401437
https://doi.org/10.1186/BF03352398
genre Fennoscandia
genre_facet Fennoscandia
op_relation Earth, Planets and Space
Scherneck, Hans-Georg, Jan M. Johansson, Martin Vermeer, James L. Davis, Glenn A. Milne, and Jerry X. Mitrovica. 2001. “BIFROST Project: 3-D Crustal Deformation Rates Derived from GPS Confirm Postglacial Rebound in Fennoscandia.” Earth, Planets and Space 53 (7): 703–8. https://doi.org/10.1186/bf03352398.
1343-8832
1880-5981
http://nrs.harvard.edu/urn-3:HUL.InstRepos:41401437
doi:10.1186/BF03352398
op_doi https://doi.org/10.1186/BF03352398
https://doi.org/10.1186/bf03352398
container_title Earth, Planets and Space
container_volume 53
container_issue 7
container_start_page 703
op_container_end_page 708
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