Helicopter vs. Volcanic Tremor: Characteristic Features of Seismic Harmonic Tremor on Volcanoes

We recorded high-frequency (> 10 Hz) harmonic tremor with spectral gliding at Hekla volcano in Iceland. Particle motion plots indicated a shallow tremor source. We observed up to two overtones beneath our Nyquist frequency of 50 Hz and could resolve a source of closely spaced pulses of very short...

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Published in:Journal of Volcanology and Geothermal Research
Main Authors: Eibl, Eva P. S., Lokmer, Ivan, Bean, Christopher J., Akelie, Eggert, Vogfjörd, Kristín S.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2015
Subjects:
Online Access:https://zenodo.org/record/53146
https://doi.org/10.1016/j.jvolgeores.2015.08.002
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spelling ftzenodo:oai:zenodo.org:53146 2023-06-06T11:54:37+02:00 Helicopter vs. Volcanic Tremor: Characteristic Features of Seismic Harmonic Tremor on Volcanoes Eibl, Eva P. S. Lokmer, Ivan Bean, Christopher J. Akelie, Eggert Vogfjörd, Kristín S. 2015-08-12 https://zenodo.org/record/53146 https://doi.org/10.1016/j.jvolgeores.2015.08.002 unknown info:eu-repo/grantAgreement/EC/FP7/308377/ https://zenodo.org/communities/ecfunded https://zenodo.org/record/53146 https://doi.org/10.1016/j.jvolgeores.2015.08.002 oai:zenodo.org:53146 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Journal of Volcanology and Geothermal Research 304 108-117 (2015) Frequency gliding Doppler shift Harmonic tremor Helicopter Volcano info:eu-repo/semantics/article publication-article 2015 ftzenodo https://doi.org/10.1016/j.jvolgeores.2015.08.002 2023-04-13T23:39:30Z We recorded high-frequency (> 10 Hz) harmonic tremor with spectral gliding at Hekla volcano in Iceland. Particle motion plots indicated a shallow tremor source. We observed up to two overtones beneath our Nyquist frequency of 50 Hz and could resolve a source of closely spaced pulses of very short duration (0.03 - 0.1 s) on zoomed seismograms. Volcanic tremor with fundamental frequencies above 5 Hz, frequency gliding and/or repetitive sources similar to our observations were observed on different volcanoes around the world. However, this frequency content, duration and occurrence of volcano-related tremor was not observed in the last 35 years of seismic observations at Hekla. Detailed analysis reveals that this tremor was related to helicopters passing the volcano. This study relates the GPS track of a helicopter with seismic recordings of the helicopter at various distances. We show the effect the distance, number of rotor blades and velocity of the helicopter has on the observed up and down glidings at up to 40 km distance. We highlight similarities and differences between volcano-related and helicopter tremor in order to help avoid misinterpretations. Article in Journal/Newspaper Hekla Iceland Zenodo Journal of Volcanology and Geothermal Research 304 108 117
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic Frequency gliding
Doppler shift
Harmonic tremor
Helicopter
Volcano
spellingShingle Frequency gliding
Doppler shift
Harmonic tremor
Helicopter
Volcano
Eibl, Eva P. S.
Lokmer, Ivan
Bean, Christopher J.
Akelie, Eggert
Vogfjörd, Kristín S.
Helicopter vs. Volcanic Tremor: Characteristic Features of Seismic Harmonic Tremor on Volcanoes
topic_facet Frequency gliding
Doppler shift
Harmonic tremor
Helicopter
Volcano
description We recorded high-frequency (> 10 Hz) harmonic tremor with spectral gliding at Hekla volcano in Iceland. Particle motion plots indicated a shallow tremor source. We observed up to two overtones beneath our Nyquist frequency of 50 Hz and could resolve a source of closely spaced pulses of very short duration (0.03 - 0.1 s) on zoomed seismograms. Volcanic tremor with fundamental frequencies above 5 Hz, frequency gliding and/or repetitive sources similar to our observations were observed on different volcanoes around the world. However, this frequency content, duration and occurrence of volcano-related tremor was not observed in the last 35 years of seismic observations at Hekla. Detailed analysis reveals that this tremor was related to helicopters passing the volcano. This study relates the GPS track of a helicopter with seismic recordings of the helicopter at various distances. We show the effect the distance, number of rotor blades and velocity of the helicopter has on the observed up and down glidings at up to 40 km distance. We highlight similarities and differences between volcano-related and helicopter tremor in order to help avoid misinterpretations.
format Article in Journal/Newspaper
author Eibl, Eva P. S.
Lokmer, Ivan
Bean, Christopher J.
Akelie, Eggert
Vogfjörd, Kristín S.
author_facet Eibl, Eva P. S.
Lokmer, Ivan
Bean, Christopher J.
Akelie, Eggert
Vogfjörd, Kristín S.
author_sort Eibl, Eva P. S.
title Helicopter vs. Volcanic Tremor: Characteristic Features of Seismic Harmonic Tremor on Volcanoes
title_short Helicopter vs. Volcanic Tremor: Characteristic Features of Seismic Harmonic Tremor on Volcanoes
title_full Helicopter vs. Volcanic Tremor: Characteristic Features of Seismic Harmonic Tremor on Volcanoes
title_fullStr Helicopter vs. Volcanic Tremor: Characteristic Features of Seismic Harmonic Tremor on Volcanoes
title_full_unstemmed Helicopter vs. Volcanic Tremor: Characteristic Features of Seismic Harmonic Tremor on Volcanoes
title_sort helicopter vs. volcanic tremor: characteristic features of seismic harmonic tremor on volcanoes
publishDate 2015
url https://zenodo.org/record/53146
https://doi.org/10.1016/j.jvolgeores.2015.08.002
genre Hekla
Iceland
genre_facet Hekla
Iceland
op_source Journal of Volcanology and Geothermal Research 304 108-117 (2015)
op_relation info:eu-repo/grantAgreement/EC/FP7/308377/
https://zenodo.org/communities/ecfunded
https://zenodo.org/record/53146
https://doi.org/10.1016/j.jvolgeores.2015.08.002
oai:zenodo.org:53146
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.1016/j.jvolgeores.2015.08.002
container_title Journal of Volcanology and Geothermal Research
container_volume 304
container_start_page 108
op_container_end_page 117
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