Vertical crustal motion observed in the BIFROST project

peer reviewed This paper reports from investigations on the robustness of estimated rates of intraplate motion from the continuous GPS project BIFROST (Baseline Inferences from Fennoscandian Rebound Observations, Sealevel and Tectonics). We study loading effects due to ocean, atmosphere and hydrolog...

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Published in:Journal of Geodynamics
Main Authors: Scherneck, Hans-Georg, Johansson, Jan M., Koivula, Hannu, VAN DAM, Tonie, Davis, James L.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science Ltd. 2003
Subjects:
GIA
GPS
Online Access:https://orbilu.uni.lu/handle/10993/832
https://doi.org/10.1016/S0264-3707(03)00005-X
id ftunivluxembourg:oai:orbilu.uni.lu:10993/832
record_format openpolar
spelling ftunivluxembourg:oai:orbilu.uni.lu:10993/832 2024-10-20T14:08:38+00:00 Vertical crustal motion observed in the BIFROST project Scherneck, Hans-Georg Johansson, Jan M. Koivula, Hannu VAN DAM, Tonie Davis, James L. 2003 https://orbilu.uni.lu/handle/10993/832 https://doi.org/10.1016/S0264-3707(03)00005-X en eng Elsevier Science Ltd. urn:issn:0264-3707 https://orbilu.uni.lu/handle/10993/832 info:hdl:10993/832 wos:000182896900004 Journal of Geodynamics, 35 (4-5), 425-441 (2003) GIA GPS sea-level tectonics Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physics Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique journal article http://purl.org/coar/resource_type/c_6501 info:eu-repo/semantics/article peer reviewed 2003 ftunivluxembourg https://doi.org/10.1016/S0264-3707(03)00005-X 2024-09-27T07:04:13Z peer reviewed This paper reports from investigations on the robustness of estimated rates of intraplate motion from the continuous GPS project BIFROST (Baseline Inferences from Fennoscandian Rebound Observations, Sealevel and Tectonics). We study loading effects due to ocean, atmosphere and hydrology and their impact on estimated rate parameters. We regularly find the admittance of a modelled perturbation at less than fifty percent of the full effect. We think that the finding relates to a difficult noise situation at all periods, and that a satisfying model for the dominating noise source has not been found yet. An additional reason for low admittance is found in the mapping process of the no-fiducial network solution into a conventional reference frame. Article in Journal/Newspaper Fennoscandian University of Luxembourg: ORBilu - Open Repository and Bibliography Journal of Geodynamics 35 4-5 425 441
institution Open Polar
collection University of Luxembourg: ORBilu - Open Repository and Bibliography
op_collection_id ftunivluxembourg
language English
topic GIA
GPS
sea-level
tectonics
Physical
chemical
mathematical & earth Sciences
Earth sciences & physical geography
Physics
Physique
chimie
mathématiques & sciences de la terre
Sciences de la terre & géographie physique
spellingShingle GIA
GPS
sea-level
tectonics
Physical
chemical
mathematical & earth Sciences
Earth sciences & physical geography
Physics
Physique
chimie
mathématiques & sciences de la terre
Sciences de la terre & géographie physique
Scherneck, Hans-Georg
Johansson, Jan M.
Koivula, Hannu
VAN DAM, Tonie
Davis, James L.
Vertical crustal motion observed in the BIFROST project
topic_facet GIA
GPS
sea-level
tectonics
Physical
chemical
mathematical & earth Sciences
Earth sciences & physical geography
Physics
Physique
chimie
mathématiques & sciences de la terre
Sciences de la terre & géographie physique
description peer reviewed This paper reports from investigations on the robustness of estimated rates of intraplate motion from the continuous GPS project BIFROST (Baseline Inferences from Fennoscandian Rebound Observations, Sealevel and Tectonics). We study loading effects due to ocean, atmosphere and hydrology and their impact on estimated rate parameters. We regularly find the admittance of a modelled perturbation at less than fifty percent of the full effect. We think that the finding relates to a difficult noise situation at all periods, and that a satisfying model for the dominating noise source has not been found yet. An additional reason for low admittance is found in the mapping process of the no-fiducial network solution into a conventional reference frame.
format Article in Journal/Newspaper
author Scherneck, Hans-Georg
Johansson, Jan M.
Koivula, Hannu
VAN DAM, Tonie
Davis, James L.
author_facet Scherneck, Hans-Georg
Johansson, Jan M.
Koivula, Hannu
VAN DAM, Tonie
Davis, James L.
author_sort Scherneck, Hans-Georg
title Vertical crustal motion observed in the BIFROST project
title_short Vertical crustal motion observed in the BIFROST project
title_full Vertical crustal motion observed in the BIFROST project
title_fullStr Vertical crustal motion observed in the BIFROST project
title_full_unstemmed Vertical crustal motion observed in the BIFROST project
title_sort vertical crustal motion observed in the bifrost project
publisher Elsevier Science Ltd.
publishDate 2003
url https://orbilu.uni.lu/handle/10993/832
https://doi.org/10.1016/S0264-3707(03)00005-X
genre Fennoscandian
genre_facet Fennoscandian
op_source Journal of Geodynamics, 35 (4-5), 425-441 (2003)
op_relation urn:issn:0264-3707
https://orbilu.uni.lu/handle/10993/832
info:hdl:10993/832
wos:000182896900004
op_doi https://doi.org/10.1016/S0264-3707(03)00005-X
container_title Journal of Geodynamics
container_volume 35
container_issue 4-5
container_start_page 425
op_container_end_page 441
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