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...
Published in: | Journal of Geodynamics |
---|---|
Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier Science Ltd.
2003
|
Subjects: | |
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 |
_version_ |
1813447831530242048 |