Detection of ice mass variation using GNSS measurements at Svalbard

We compare observed uplift rates of Global Navigation Satellite Systems (GNSS) with geophysical predictions at sites located on Spitsbergen. We show here that using modern postglacial rebound models, realistic mass balance for Present Day Ice Melting (PDIM) and taking the deglaciation of the Little...

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Published in:Journal of Geodynamics
Main Author: Rajner, Marcin
Language:unknown
Published: 2018
Subjects:
Online Access:https://doi.org/10.1016/j.jog.2018.06.001
https://research.chalmers.se/en/publication/505045
id ftchalmersuniv:oai:research.chalmers.se:505045
record_format openpolar
spelling ftchalmersuniv:oai:research.chalmers.se:505045 2023-05-15T16:34:56+02:00 Detection of ice mass variation using GNSS measurements at Svalbard Rajner, Marcin 2018 text https://doi.org/10.1016/j.jog.2018.06.001 https://research.chalmers.se/en/publication/505045 unknown http://dx.doi.org/10.1016/j.jog.2018.06.001 https://research.chalmers.se/en/publication/505045 Other Earth and Related Environmental Sciences Geophysics Geochemistry Loading deformations present day ice melting GNSS mass balance glacial isostatic adjustment Svalbard 2018 ftchalmersuniv https://doi.org/10.1016/j.jog.2018.06.001 2022-12-11T07:08:07Z We compare observed uplift rates of Global Navigation Satellite Systems (GNSS) with geophysical predictions at sites located on Spitsbergen. We show here that using modern postglacial rebound models, realistic mass balance for Present Day Ice Melting (PDIM) and taking the deglaciation of the Little Ice Age (LIA) into account, we can close the overall uplift budget at a level of a few millimetres per year. For this study we used GNSS data from well-established geodetic sites in Ny-Ålesund and the new data from Hornsund. The significant increase of uplift rates since the beginning of 2011 was observed at both gnss sites. These height changes are attributed to recent increased ice mass loss of 6.0 Gt yr−1 for Svalbard. The total mass loss is estimated at 14.7 Gt yr−1. Ice unloading caused also a noticeable increase of distance between Ny-Ålesund and Hornsund. We show that the specific location of the two sites facilitates inference of differential mass loss within the Svalbard Archipelago. Other/Unknown Material Hornsund Ny Ålesund Ny-Ålesund Svalbard Spitsbergen Chalmers University of Technology: Chalmers research Hornsund ENVELOPE(15.865,15.865,76.979,76.979) Ny-Ålesund Svalbard Svalbard Archipelago Journal of Geodynamics 121 20 25
institution Open Polar
collection Chalmers University of Technology: Chalmers research
op_collection_id ftchalmersuniv
language unknown
topic Other Earth and Related Environmental Sciences
Geophysics
Geochemistry
Loading deformations
present day ice melting
GNSS
mass balance
glacial isostatic adjustment
Svalbard
spellingShingle Other Earth and Related Environmental Sciences
Geophysics
Geochemistry
Loading deformations
present day ice melting
GNSS
mass balance
glacial isostatic adjustment
Svalbard
Rajner, Marcin
Detection of ice mass variation using GNSS measurements at Svalbard
topic_facet Other Earth and Related Environmental Sciences
Geophysics
Geochemistry
Loading deformations
present day ice melting
GNSS
mass balance
glacial isostatic adjustment
Svalbard
description We compare observed uplift rates of Global Navigation Satellite Systems (GNSS) with geophysical predictions at sites located on Spitsbergen. We show here that using modern postglacial rebound models, realistic mass balance for Present Day Ice Melting (PDIM) and taking the deglaciation of the Little Ice Age (LIA) into account, we can close the overall uplift budget at a level of a few millimetres per year. For this study we used GNSS data from well-established geodetic sites in Ny-Ålesund and the new data from Hornsund. The significant increase of uplift rates since the beginning of 2011 was observed at both gnss sites. These height changes are attributed to recent increased ice mass loss of 6.0 Gt yr−1 for Svalbard. The total mass loss is estimated at 14.7 Gt yr−1. Ice unloading caused also a noticeable increase of distance between Ny-Ålesund and Hornsund. We show that the specific location of the two sites facilitates inference of differential mass loss within the Svalbard Archipelago.
author Rajner, Marcin
author_facet Rajner, Marcin
author_sort Rajner, Marcin
title Detection of ice mass variation using GNSS measurements at Svalbard
title_short Detection of ice mass variation using GNSS measurements at Svalbard
title_full Detection of ice mass variation using GNSS measurements at Svalbard
title_fullStr Detection of ice mass variation using GNSS measurements at Svalbard
title_full_unstemmed Detection of ice mass variation using GNSS measurements at Svalbard
title_sort detection of ice mass variation using gnss measurements at svalbard
publishDate 2018
url https://doi.org/10.1016/j.jog.2018.06.001
https://research.chalmers.se/en/publication/505045
long_lat ENVELOPE(15.865,15.865,76.979,76.979)
geographic Hornsund
Ny-Ålesund
Svalbard
Svalbard Archipelago
geographic_facet Hornsund
Ny-Ålesund
Svalbard
Svalbard Archipelago
genre Hornsund
Ny Ålesund
Ny-Ålesund
Svalbard
Spitsbergen
genre_facet Hornsund
Ny Ålesund
Ny-Ålesund
Svalbard
Spitsbergen
op_relation http://dx.doi.org/10.1016/j.jog.2018.06.001
https://research.chalmers.se/en/publication/505045
op_doi https://doi.org/10.1016/j.jog.2018.06.001
container_title Journal of Geodynamics
container_volume 121
container_start_page 20
op_container_end_page 25
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