Automating long-term glacier dynamics monitoring using single-station seismological observations and fuzzy logic classification: a case study from Spitsbergen

Retreating glaciers are a consequence of a warming climate. Thus, numerous monitoring campaigns are being carried out to increase understanding of this on-going process. One phenomenon related to dynamic glacial changes is glacier-induced seismicity; however, weak seismic events are difficult to rec...

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Main Authors: W. GAJEK, J. TROJANOWSKI, M. MALINOWSKI
Format: Article
Language:English
Published: Cambridge University Press 2017-08-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143017000259/type/journal_article
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author W. GAJEK
J. TROJANOWSKI
M. MALINOWSKI
author_facet W. GAJEK
J. TROJANOWSKI
M. MALINOWSKI
author_sort W. GAJEK
collection DOAJ
description Retreating glaciers are a consequence of a warming climate. Thus, numerous monitoring campaigns are being carried out to increase understanding of this on-going process. One phenomenon related to dynamic glacial changes is glacier-induced seismicity; however, weak seismic events are difficult to record due to the sparse seismological network in arctic areas. We have developed an automatic procedure capable of detecting glacier-induced seismic events using records from a single permanent seismological station. To distinguish between glacial and non-glacial signals, we developed a fuzzy logic algorithm based on the signal frequency and energy flow analysis. We studied the long-term changes in glacier-induced seismicity in Hornsund (southern Spitsbergen) and in Kongsfjorden (western Spitsbergen). We found that the number of detected glacial-origin events in the Hornsund dataset over the years 2013-14 has doubled. In the Kongsfjorden dataset, we observed a steady increase in the number of glacier-induced events with each year. We also observed that the seasonal event distribution correlates best with 1 month lagged temperatures, and that extreme rain events can intensify seismic emissions. Our study demonstrates the possibility of using long-term seismological observations from a single permanent station to automatically monitor the dynamic activity of nearby glaciers and retrieve its characteristic features.
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spelling doaj.art-21f89129387c41d3a64e9f1999101f052023-03-09T12:40:27ZengCambridge University PressJournal of Glaciology0022-14301727-56522017-08-016358159210.1017/jog.2017.25Automating long-term glacier dynamics monitoring using single-station seismological observations and fuzzy logic classification: a case study from SpitsbergenW. GAJEK0https://orcid.org/0000-0002-8754-3440J. TROJANOWSKI1M. MALINOWSKI2Institute of Geophysics, Polish Academy of Sciences, Warsaw, PolandInstitute of Geophysics, Polish Academy of Sciences, Warsaw, PolandInstitute of Geophysics, Polish Academy of Sciences, Warsaw, PolandRetreating glaciers are a consequence of a warming climate. Thus, numerous monitoring campaigns are being carried out to increase understanding of this on-going process. One phenomenon related to dynamic glacial changes is glacier-induced seismicity; however, weak seismic events are difficult to record due to the sparse seismological network in arctic areas. We have developed an automatic procedure capable of detecting glacier-induced seismic events using records from a single permanent seismological station. To distinguish between glacial and non-glacial signals, we developed a fuzzy logic algorithm based on the signal frequency and energy flow analysis. We studied the long-term changes in glacier-induced seismicity in Hornsund (southern Spitsbergen) and in Kongsfjorden (western Spitsbergen). We found that the number of detected glacial-origin events in the Hornsund dataset over the years 2013-14 has doubled. In the Kongsfjorden dataset, we observed a steady increase in the number of glacier-induced events with each year. We also observed that the seasonal event distribution correlates best with 1 month lagged temperatures, and that extreme rain events can intensify seismic emissions. Our study demonstrates the possibility of using long-term seismological observations from a single permanent station to automatically monitor the dynamic activity of nearby glaciers and retrieve its characteristic features.https://www.cambridge.org/core/product/identifier/S0022143017000259/type/journal_articlecalvingglacier geophysicsglacier monitoringseismology
spellingShingle W. GAJEK
J. TROJANOWSKI
M. MALINOWSKI
Automating long-term glacier dynamics monitoring using single-station seismological observations and fuzzy logic classification: a case study from Spitsbergen
Journal of Glaciology
calving
glacier geophysics
glacier monitoring
seismology
title Automating long-term glacier dynamics monitoring using single-station seismological observations and fuzzy logic classification: a case study from Spitsbergen
title_full Automating long-term glacier dynamics monitoring using single-station seismological observations and fuzzy logic classification: a case study from Spitsbergen
title_fullStr Automating long-term glacier dynamics monitoring using single-station seismological observations and fuzzy logic classification: a case study from Spitsbergen
title_full_unstemmed Automating long-term glacier dynamics monitoring using single-station seismological observations and fuzzy logic classification: a case study from Spitsbergen
title_short Automating long-term glacier dynamics monitoring using single-station seismological observations and fuzzy logic classification: a case study from Spitsbergen
title_sort automating long term glacier dynamics monitoring using single station seismological observations and fuzzy logic classification a case study from spitsbergen
topic calving
glacier geophysics
glacier monitoring
seismology
url https://www.cambridge.org/core/product/identifier/S0022143017000259/type/journal_article
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