Dynamical changes of seismic properties prior to, during, and after 2014–2015 Holuhraun Eruption, Iceland

In volcanic eruption monitoring, it is urgent to promptly detect changes in the volcanic system during the crisis period. Ideally continuous, temporally high-resolution, multidisciplinary data is available for this. However, some volcanoes are only being monitored using a single discipline or a sing...

Full description

Bibliographic Details
Main Authors: Sudibyo, Maria R.P., Eibl, Eva P. S., Hainzl, Sebastian, Ohrnberger, Matthias
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2024-1445
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1445/
id ftcopernicus:oai:publications.copernicus.org:egusphere120272
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:egusphere120272 2024-06-23T07:53:58+00:00 Dynamical changes of seismic properties prior to, during, and after 2014–2015 Holuhraun Eruption, Iceland Sudibyo, Maria R.P. Eibl, Eva P. S. Hainzl, Sebastian Ohrnberger, Matthias 2024-06-04 application/pdf https://doi.org/10.5194/egusphere-2024-1445 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1445/ eng eng doi:10.5194/egusphere-2024-1445 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1445/ eISSN: Text 2024 ftcopernicus https://doi.org/10.5194/egusphere-2024-1445 2024-06-13T01:24:17Z In volcanic eruption monitoring, it is urgent to promptly detect changes in the volcanic system during the crisis period. Ideally continuous, temporally high-resolution, multidisciplinary data is available for this. However, some volcanoes are only being monitored using a single discipline or a single seismic station. In this case, it makes sense to harvest information from the available limited data set with several different techniques. Changes in the seismic complexity could reveal the dynamic changes due to magma propagation. We tested the performance of Permutation Entropy (PE) and Phase Permutation Entropy (PPE), which are fast and robust quantification of time series complexity, to monitor the change in the eruption process of 2014–2015 Holuhraun in Iceland. We additionally calculated the instantaneous frequency (IF), which is commonly used to monitor the frequency changes in a non-stationary signal. We observed distinct changes in the temporal variation of PE, PPE, and IF, which are consistent with the changing state from quiescence to magma propagation and then to eruption. During the eruption, PE and PPE fit the lava discharge rate, showing their potential to forecast the duration of the eruption. Finally, we also assessed the influence of the atmospheric noise to be considered in eruption monitoring. Text Iceland Copernicus Publications: E-Journals Holuhraun ENVELOPE(-16.831,-16.831,64.852,64.852)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description In volcanic eruption monitoring, it is urgent to promptly detect changes in the volcanic system during the crisis period. Ideally continuous, temporally high-resolution, multidisciplinary data is available for this. However, some volcanoes are only being monitored using a single discipline or a single seismic station. In this case, it makes sense to harvest information from the available limited data set with several different techniques. Changes in the seismic complexity could reveal the dynamic changes due to magma propagation. We tested the performance of Permutation Entropy (PE) and Phase Permutation Entropy (PPE), which are fast and robust quantification of time series complexity, to monitor the change in the eruption process of 2014–2015 Holuhraun in Iceland. We additionally calculated the instantaneous frequency (IF), which is commonly used to monitor the frequency changes in a non-stationary signal. We observed distinct changes in the temporal variation of PE, PPE, and IF, which are consistent with the changing state from quiescence to magma propagation and then to eruption. During the eruption, PE and PPE fit the lava discharge rate, showing their potential to forecast the duration of the eruption. Finally, we also assessed the influence of the atmospheric noise to be considered in eruption monitoring.
format Text
author Sudibyo, Maria R.P.
Eibl, Eva P. S.
Hainzl, Sebastian
Ohrnberger, Matthias
spellingShingle Sudibyo, Maria R.P.
Eibl, Eva P. S.
Hainzl, Sebastian
Ohrnberger, Matthias
Dynamical changes of seismic properties prior to, during, and after 2014–2015 Holuhraun Eruption, Iceland
author_facet Sudibyo, Maria R.P.
Eibl, Eva P. S.
Hainzl, Sebastian
Ohrnberger, Matthias
author_sort Sudibyo, Maria R.P.
title Dynamical changes of seismic properties prior to, during, and after 2014–2015 Holuhraun Eruption, Iceland
title_short Dynamical changes of seismic properties prior to, during, and after 2014–2015 Holuhraun Eruption, Iceland
title_full Dynamical changes of seismic properties prior to, during, and after 2014–2015 Holuhraun Eruption, Iceland
title_fullStr Dynamical changes of seismic properties prior to, during, and after 2014–2015 Holuhraun Eruption, Iceland
title_full_unstemmed Dynamical changes of seismic properties prior to, during, and after 2014–2015 Holuhraun Eruption, Iceland
title_sort dynamical changes of seismic properties prior to, during, and after 2014–2015 holuhraun eruption, iceland
publishDate 2024
url https://doi.org/10.5194/egusphere-2024-1445
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1445/
long_lat ENVELOPE(-16.831,-16.831,64.852,64.852)
geographic Holuhraun
geographic_facet Holuhraun
genre Iceland
genre_facet Iceland
op_source eISSN:
op_relation doi:10.5194/egusphere-2024-1445
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1445/
op_doi https://doi.org/10.5194/egusphere-2024-1445
_version_ 1802645883018280960