Permafrost dynamics at Mt. Zugspitze from passive seismic monitoring

Degradation of mountain permafrost in response to global warming reduces the stability of steep rock slopes, which increases the hazard potential. However, continuous monitoring of permafrost environments remains challenging due to the harsh conditions typically encountered in high Alpine terrain. H...

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Main Authors: Lindner, F., Scandroglio, R., Smolinski, K., Fichtner, A., Wassermann, J.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018413
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018413 2023-07-02T03:33:25+02:00 Permafrost dynamics at Mt. Zugspitze from passive seismic monitoring Lindner, F. Scandroglio, R. Smolinski, K. Fichtner, A. Wassermann, J. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018413 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2344 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018413 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-2344 2023-06-11T23:39:54Z Degradation of mountain permafrost in response to global warming reduces the stability of steep rock slopes, which increases the hazard potential. However, continuous monitoring of permafrost environments remains challenging due to the harsh conditions typically encountered in high Alpine terrain. Here, we present results from passive seismic monitoring of permafrost at Mt. Zugspitze in the German/Austrian Alps. Single-station coda-wave interferometry reveals seasonal freeze-thaw cycles and permafrost degradation over the past 17 years, consistent with modeled velocity changes using temperature logs from a nearby borehole. To constrain the location of these changes, we installed three small seismic arrays along the ridge of Mt. Zugspitze in summer/fall 2021 and exploit the cable car operations at the summit as stationary noise sources for direct wave monitoring between the deployment sites. The results suggest that significant seasonal freeze-thaw cycles associated with permafrost bodies only occur in the western part of the ridge, which is also favored by thermal modeling. To further pinpoint the presence of permafrost, we repeatedly employ distributed acoustic sensing along the ridge, which allows us to sense seismic wave propagation on a meter-scale. In addition to the thermal rock properties, we find that the seismic velocity is sensitive to the presence of cleft water, which may critically contribute to the stability of rock walls. In contrast to more classical methods like borehole temperature logging and electrical resistivity monitoring, seismology combines high temporal resolution and spatial insights over comparatively large areas and thus constitutes a valuable contribution to permafrost monitoring. Conference Object permafrost GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description Degradation of mountain permafrost in response to global warming reduces the stability of steep rock slopes, which increases the hazard potential. However, continuous monitoring of permafrost environments remains challenging due to the harsh conditions typically encountered in high Alpine terrain. Here, we present results from passive seismic monitoring of permafrost at Mt. Zugspitze in the German/Austrian Alps. Single-station coda-wave interferometry reveals seasonal freeze-thaw cycles and permafrost degradation over the past 17 years, consistent with modeled velocity changes using temperature logs from a nearby borehole. To constrain the location of these changes, we installed three small seismic arrays along the ridge of Mt. Zugspitze in summer/fall 2021 and exploit the cable car operations at the summit as stationary noise sources for direct wave monitoring between the deployment sites. The results suggest that significant seasonal freeze-thaw cycles associated with permafrost bodies only occur in the western part of the ridge, which is also favored by thermal modeling. To further pinpoint the presence of permafrost, we repeatedly employ distributed acoustic sensing along the ridge, which allows us to sense seismic wave propagation on a meter-scale. In addition to the thermal rock properties, we find that the seismic velocity is sensitive to the presence of cleft water, which may critically contribute to the stability of rock walls. In contrast to more classical methods like borehole temperature logging and electrical resistivity monitoring, seismology combines high temporal resolution and spatial insights over comparatively large areas and thus constitutes a valuable contribution to permafrost monitoring.
format Conference Object
author Lindner, F.
Scandroglio, R.
Smolinski, K.
Fichtner, A.
Wassermann, J.
spellingShingle Lindner, F.
Scandroglio, R.
Smolinski, K.
Fichtner, A.
Wassermann, J.
Permafrost dynamics at Mt. Zugspitze from passive seismic monitoring
author_facet Lindner, F.
Scandroglio, R.
Smolinski, K.
Fichtner, A.
Wassermann, J.
author_sort Lindner, F.
title Permafrost dynamics at Mt. Zugspitze from passive seismic monitoring
title_short Permafrost dynamics at Mt. Zugspitze from passive seismic monitoring
title_full Permafrost dynamics at Mt. Zugspitze from passive seismic monitoring
title_fullStr Permafrost dynamics at Mt. Zugspitze from passive seismic monitoring
title_full_unstemmed Permafrost dynamics at Mt. Zugspitze from passive seismic monitoring
title_sort permafrost dynamics at mt. zugspitze from passive seismic monitoring
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018413
genre permafrost
genre_facet permafrost
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2344
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018413
op_doi https://doi.org/10.57757/IUGG23-2344
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