Case study of combined marine- and land-based passive seismic surveying in front of Nordenskiöldbreen outlet glacier, Adolfbukta, Svalbard

Glaciers generate seismic waves due to calving and fracturing, meaning that recording and following event classification can be used to monitor glacier dynamics. Our aim with this study is to analyse seismic data acquired at the seabed and on land in front of Nordenskiöldbreen on Svalbard during 8 d...

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Published in:Near Surface Geophysics
Main Authors: Stemland, Helene, Ruud, Bent Ole, Johansen, Tor Arne
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://hdl.handle.net/11250/3092711
https://doi.org/10.1002/nsg.12266
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spelling ftunivbergen:oai:bora.uib.no:11250/3092711 2023-10-29T02:36:31+01:00 Case study of combined marine- and land-based passive seismic surveying in front of Nordenskiöldbreen outlet glacier, Adolfbukta, Svalbard Stemland, Helene Ruud, Bent Ole Johansen, Tor Arne 2023 application/pdf https://hdl.handle.net/11250/3092711 https://doi.org/10.1002/nsg.12266 eng eng Wiley urn:issn:1569-4445 https://hdl.handle.net/11250/3092711 https://doi.org/10.1002/nsg.12266 cristin:2177697 Near Surface Geophysics. 2023, 21 (5), 376-391. Navngivelse-Ikkekommersiell 4.0 Internasjonal http://creativecommons.org/licenses/by-nc/4.0/deed.no Copyright 2023 The Author(s) Near Surface Geophysics 376-391 21 5 Journal article Peer reviewed 2023 ftunivbergen https://doi.org/10.1002/nsg.12266 2023-10-04T23:08:15Z Glaciers generate seismic waves due to calving and fracturing, meaning that recording and following event classification can be used to monitor glacier dynamics. Our aim with this study is to analyse seismic data acquired at the seabed and on land in front of Nordenskiöldbreen on Svalbard during 8 days in October 2020. The survey included 27 ocean bottom nodes, each equipped with 3 geophones and a hydrophone, and 101 land-based geophones. The resulting data contain numerous seismic P-, S- and Scholte wave events throughout the study period, as well as non-seismic gravity waves. The recording quality strongly depends on receiver type and location, especially for the latter wave types. Our results demonstrate that hydrophones at the seabed are advantageous to record gravity waves, and that Scholte waves are only recorded close to the glacier. The Scholte waves are used to estimate the near-surface S-wave profile of the seabed sediments, and the gravity wave amplitudes are converted to wave heights at the surface. We further discuss possible source mechanisms for the recorded events and present evidence that waves from earthquakes, calving and brittle fracturing of the glacier and icebergs are all represented in the data. The interpretation is based on frequency content, duration, seismic velocities and onset (emergent/impulsive) and is supported by source localization, which we show is challenging for this dataset. In conclusion, our study demonstrates the potential of using seismic observations for detecting glacier-related events and provides valuable knowledge about the importance of survey geometry, particularly the advantages of including seabed receivers in the vicinity of the glacier. publishedVersion Article in Journal/Newspaper glacier Svalbard University of Bergen: Bergen Open Research Archive (BORA-UiB) Near Surface Geophysics 21 5 376 391
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
description Glaciers generate seismic waves due to calving and fracturing, meaning that recording and following event classification can be used to monitor glacier dynamics. Our aim with this study is to analyse seismic data acquired at the seabed and on land in front of Nordenskiöldbreen on Svalbard during 8 days in October 2020. The survey included 27 ocean bottom nodes, each equipped with 3 geophones and a hydrophone, and 101 land-based geophones. The resulting data contain numerous seismic P-, S- and Scholte wave events throughout the study period, as well as non-seismic gravity waves. The recording quality strongly depends on receiver type and location, especially for the latter wave types. Our results demonstrate that hydrophones at the seabed are advantageous to record gravity waves, and that Scholte waves are only recorded close to the glacier. The Scholte waves are used to estimate the near-surface S-wave profile of the seabed sediments, and the gravity wave amplitudes are converted to wave heights at the surface. We further discuss possible source mechanisms for the recorded events and present evidence that waves from earthquakes, calving and brittle fracturing of the glacier and icebergs are all represented in the data. The interpretation is based on frequency content, duration, seismic velocities and onset (emergent/impulsive) and is supported by source localization, which we show is challenging for this dataset. In conclusion, our study demonstrates the potential of using seismic observations for detecting glacier-related events and provides valuable knowledge about the importance of survey geometry, particularly the advantages of including seabed receivers in the vicinity of the glacier. publishedVersion
format Article in Journal/Newspaper
author Stemland, Helene
Ruud, Bent Ole
Johansen, Tor Arne
spellingShingle Stemland, Helene
Ruud, Bent Ole
Johansen, Tor Arne
Case study of combined marine- and land-based passive seismic surveying in front of Nordenskiöldbreen outlet glacier, Adolfbukta, Svalbard
author_facet Stemland, Helene
Ruud, Bent Ole
Johansen, Tor Arne
author_sort Stemland, Helene
title Case study of combined marine- and land-based passive seismic surveying in front of Nordenskiöldbreen outlet glacier, Adolfbukta, Svalbard
title_short Case study of combined marine- and land-based passive seismic surveying in front of Nordenskiöldbreen outlet glacier, Adolfbukta, Svalbard
title_full Case study of combined marine- and land-based passive seismic surveying in front of Nordenskiöldbreen outlet glacier, Adolfbukta, Svalbard
title_fullStr Case study of combined marine- and land-based passive seismic surveying in front of Nordenskiöldbreen outlet glacier, Adolfbukta, Svalbard
title_full_unstemmed Case study of combined marine- and land-based passive seismic surveying in front of Nordenskiöldbreen outlet glacier, Adolfbukta, Svalbard
title_sort case study of combined marine- and land-based passive seismic surveying in front of nordenskiöldbreen outlet glacier, adolfbukta, svalbard
publisher Wiley
publishDate 2023
url https://hdl.handle.net/11250/3092711
https://doi.org/10.1002/nsg.12266
genre glacier
Svalbard
genre_facet glacier
Svalbard
op_source Near Surface Geophysics
376-391
21
5
op_relation urn:issn:1569-4445
https://hdl.handle.net/11250/3092711
https://doi.org/10.1002/nsg.12266
cristin:2177697
Near Surface Geophysics. 2023, 21 (5), 376-391.
op_rights Navngivelse-Ikkekommersiell 4.0 Internasjonal
http://creativecommons.org/licenses/by-nc/4.0/deed.no
Copyright 2023 The Author(s)
op_doi https://doi.org/10.1002/nsg.12266
container_title Near Surface Geophysics
container_volume 21
container_issue 5
container_start_page 376
op_container_end_page 391
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