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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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 |
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DataCite Metadata Store (German National Library of Science and Technology) |
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<!--!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 |
_version_ |
1772187080890253312 |