Recent results based on continuous GPS observations of the GIA process in Fennoscandia from BIFROST

We present the latest 3D velocity field of the Fennoscandian glacial isostatic adjustment (GIA) processfrom BIFROST. It is derived from more than 4800 days (13 years) of data at more than 80 permanentGPS sites. We use the GAMIT/GLOBK and the GIPSY/OASIS II software packages for GPS analysis andcompa...

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Published in:Journal of Geodynamics
Main Authors: Lidberg, Martin, Johansson, Jan, Scherneck, Hans-Georg, Milne, Glenn A.
Language:unknown
Published: 2010
Subjects:
Online Access:https://doi.org/10.1016/j.jog.2009.11.010
https://research.chalmers.se/en/publication/120398
id ftchalmersuniv:oai:research.chalmers.se:120398
record_format openpolar
spelling ftchalmersuniv:oai:research.chalmers.se:120398 2023-05-15T16:11:54+02:00 Recent results based on continuous GPS observations of the GIA process in Fennoscandia from BIFROST Lidberg, Martin Johansson, Jan Scherneck, Hans-Georg Milne, Glenn A. 2010 text https://doi.org/10.1016/j.jog.2009.11.010 https://research.chalmers.se/en/publication/120398 unknown http://dx.doi.org/10.1016/j.jog.2009.11.010 https://research.chalmers.se/en/publication/120398 Other Earth and Related Environmental Sciences solid earth deformation Glacial isostasy Satellite geodesy 2010 ftchalmersuniv https://doi.org/10.1016/j.jog.2009.11.010 2022-12-11T07:09:52Z We present the latest 3D velocity field of the Fennoscandian glacial isostatic adjustment (GIA) processfrom BIFROST. It is derived from more than 4800 days (13 years) of data at more than 80 permanentGPS sites. We use the GAMIT/GLOBK and the GIPSY/OASIS II software packages for GPS analysis andcompare the results. The solution has an internal accuracy at the level of 0.2 mm/year (1 sigma) forhorizontal velocities at the best sites.Wealso present a revised GIA prediction model. At the best sites, theoptimal model agrees with the observations to within 0.4 mm/year. However, the model systematicallyoverpredicts the magnitude of horizontal rates in the north. We discuss limitations in computed andpresented GNSS station velocities, where especially possible instability over time causing non-linearpattern in vertical time series are considered. In extension, preliminary results from an investigationapplying revised analysis strategies on a sparse subset of the database are presented, indicating possibleimprovements for the future. Other/Unknown Material Fennoscandia Fennoscandian Chalmers University of Technology: Chalmers research Journal of Geodynamics 50 1 8 18
institution Open Polar
collection Chalmers University of Technology: Chalmers research
op_collection_id ftchalmersuniv
language unknown
topic Other Earth and Related Environmental Sciences
solid earth deformation
Glacial isostasy
Satellite geodesy
spellingShingle Other Earth and Related Environmental Sciences
solid earth deformation
Glacial isostasy
Satellite geodesy
Lidberg, Martin
Johansson, Jan
Scherneck, Hans-Georg
Milne, Glenn A.
Recent results based on continuous GPS observations of the GIA process in Fennoscandia from BIFROST
topic_facet Other Earth and Related Environmental Sciences
solid earth deformation
Glacial isostasy
Satellite geodesy
description We present the latest 3D velocity field of the Fennoscandian glacial isostatic adjustment (GIA) processfrom BIFROST. It is derived from more than 4800 days (13 years) of data at more than 80 permanentGPS sites. We use the GAMIT/GLOBK and the GIPSY/OASIS II software packages for GPS analysis andcompare the results. The solution has an internal accuracy at the level of 0.2 mm/year (1 sigma) forhorizontal velocities at the best sites.Wealso present a revised GIA prediction model. At the best sites, theoptimal model agrees with the observations to within 0.4 mm/year. However, the model systematicallyoverpredicts the magnitude of horizontal rates in the north. We discuss limitations in computed andpresented GNSS station velocities, where especially possible instability over time causing non-linearpattern in vertical time series are considered. In extension, preliminary results from an investigationapplying revised analysis strategies on a sparse subset of the database are presented, indicating possibleimprovements for the future.
author Lidberg, Martin
Johansson, Jan
Scherneck, Hans-Georg
Milne, Glenn A.
author_facet Lidberg, Martin
Johansson, Jan
Scherneck, Hans-Georg
Milne, Glenn A.
author_sort Lidberg, Martin
title Recent results based on continuous GPS observations of the GIA process in Fennoscandia from BIFROST
title_short Recent results based on continuous GPS observations of the GIA process in Fennoscandia from BIFROST
title_full Recent results based on continuous GPS observations of the GIA process in Fennoscandia from BIFROST
title_fullStr Recent results based on continuous GPS observations of the GIA process in Fennoscandia from BIFROST
title_full_unstemmed Recent results based on continuous GPS observations of the GIA process in Fennoscandia from BIFROST
title_sort recent results based on continuous gps observations of the gia process in fennoscandia from bifrost
publishDate 2010
url https://doi.org/10.1016/j.jog.2009.11.010
https://research.chalmers.se/en/publication/120398
genre Fennoscandia
Fennoscandian
genre_facet Fennoscandia
Fennoscandian
op_relation http://dx.doi.org/10.1016/j.jog.2009.11.010
https://research.chalmers.se/en/publication/120398
op_doi https://doi.org/10.1016/j.jog.2009.11.010
container_title Journal of Geodynamics
container_volume 50
container_issue 1
container_start_page 8
op_container_end_page 18
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