Cryoseismicity triggered by ice mass discharge through the Antarctic subglacial hydrographic network ...

<!--!introduction!--> We analyze seismic time series collected during experimental campaigns in the area of the David Glacier, South Victoria Land, Antarctica, between 2003 and 2016. We observe hundreds of repeating seismic events, characterized by highly correlated waveforms (cross-correlatio...

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Main Authors: Danesi, Stefania, Borghi, Alessandra, Salimbeni, Simone, Urbini, Stefano, Frezzotti, Massimo
Format: Conference Object
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-3899
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020647
id ftdatacite:10.57757/iugg23-3899
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spelling ftdatacite:10.57757/iugg23-3899 2023-07-23T04:14:45+02:00 Cryoseismicity triggered by ice mass discharge through the Antarctic subglacial hydrographic network ... Danesi, Stefania Borghi, Alessandra Salimbeni, Simone Urbini, Stefano Frezzotti, Massimo 2023 https://dx.doi.org/10.57757/iugg23-3899 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020647 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-3899 2023-07-03T22:00:45Z <!--!introduction!--> We analyze seismic time series collected during experimental campaigns in the area of the David Glacier, South Victoria Land, Antarctica, between 2003 and 2016. We observe hundreds of repeating seismic events, characterized by highly correlated waveforms (cross-correlation > 0.95), which mainly occur in the floating area between the grounding and the floating line of the ice stream. The joint analysis of seismic occurrences and observed local tide measurements shows that seismicity is not triggered by a seasonal, periodic forcing such as the ocean tide, but more likely by transient irregular impulses. We consider possible environmental processes and their impact on the coupling between the glacier flow and the brittle bedrock failure. Our results suggest that clustered and repeated seismic events may be correlated with transient episodes of mass ice discharge (observed by satellite GRACE and GRACE-FO experiments) through the subglacial hydrographic system that originates ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Antarc* Antarctic Antarctica David Glacier Victoria Land DataCite Metadata Store (German National Library of Science and Technology) Antarctic David Glacier ENVELOPE(160.000,160.000,-75.333,-75.333) The Antarctic Victoria Land
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description <!--!introduction!--> We analyze seismic time series collected during experimental campaigns in the area of the David Glacier, South Victoria Land, Antarctica, between 2003 and 2016. We observe hundreds of repeating seismic events, characterized by highly correlated waveforms (cross-correlation > 0.95), which mainly occur in the floating area between the grounding and the floating line of the ice stream. The joint analysis of seismic occurrences and observed local tide measurements shows that seismicity is not triggered by a seasonal, periodic forcing such as the ocean tide, but more likely by transient irregular impulses. We consider possible environmental processes and their impact on the coupling between the glacier flow and the brittle bedrock failure. Our results suggest that clustered and repeated seismic events may be correlated with transient episodes of mass ice discharge (observed by satellite GRACE and GRACE-FO experiments) through the subglacial hydrographic system that originates ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...
format Conference Object
author Danesi, Stefania
Borghi, Alessandra
Salimbeni, Simone
Urbini, Stefano
Frezzotti, Massimo
spellingShingle Danesi, Stefania
Borghi, Alessandra
Salimbeni, Simone
Urbini, Stefano
Frezzotti, Massimo
Cryoseismicity triggered by ice mass discharge through the Antarctic subglacial hydrographic network ...
author_facet Danesi, Stefania
Borghi, Alessandra
Salimbeni, Simone
Urbini, Stefano
Frezzotti, Massimo
author_sort Danesi, Stefania
title Cryoseismicity triggered by ice mass discharge through the Antarctic subglacial hydrographic network ...
title_short Cryoseismicity triggered by ice mass discharge through the Antarctic subglacial hydrographic network ...
title_full Cryoseismicity triggered by ice mass discharge through the Antarctic subglacial hydrographic network ...
title_fullStr Cryoseismicity triggered by ice mass discharge through the Antarctic subglacial hydrographic network ...
title_full_unstemmed Cryoseismicity triggered by ice mass discharge through the Antarctic subglacial hydrographic network ...
title_sort cryoseismicity triggered by ice mass discharge through the antarctic subglacial hydrographic network ...
publisher GFZ German Research Centre for Geosciences
publishDate 2023
url https://dx.doi.org/10.57757/iugg23-3899
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020647
long_lat ENVELOPE(160.000,160.000,-75.333,-75.333)
geographic Antarctic
David Glacier
The Antarctic
Victoria Land
geographic_facet Antarctic
David Glacier
The Antarctic
Victoria Land
genre Antarc*
Antarctic
Antarctica
David Glacier
Victoria Land
genre_facet Antarc*
Antarctic
Antarctica
David Glacier
Victoria Land
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.57757/iugg23-3899
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