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.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2015
Subjects:
Online Access:http://hdl.handle.net/10197/7005
https://doi.org/10.1016/j.jvolgeores.2015.08.002
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spelling ftunivcolldublin:oai:researchrepository.ucd.ie:10197/7005 2023-05-15T16:34:02+02:00 Helicopter vs. volcanic tremor: Characteristic features of seismic harmonic tremor on volcanoes Eibl, Eva P. S. Lokmer, Ivan Bean, Christopher J. 2015-09-10T10:13:15Z http://hdl.handle.net/10197/7005 https://doi.org/10.1016/j.jvolgeores.2015.08.002 en eng Elsevier Journal of Volcanology and Geothermal Research http://hdl.handle.net/10197/7005 304 108 117 doi:10.1016/j.jvolgeores.2015.08.002 This is the author’s version of a work that was accepted for publication in Journal of Volcanology and Geothermal Research. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Journal of Volcanology and Geothermal Research (VOL 304, ISSUE 2015, (2015)) DOI:10.1016/j.jvolgeores.2015.08.002 Frequency gliding Doppler shift Harmonic tremor Helicopter Volcano Journal Article 2015 ftunivcolldublin https://doi.org/10.1016/j.jvolgeores.2015.08.002 2022-04-08T14:18:40Z 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. European Commission - Seventh Framework Programme (FP7) Article in Journal/Newspaper Hekla Iceland University College Dublin: Research Repository UCD Journal of Volcanology and Geothermal Research 304 108 117
institution Open Polar
collection University College Dublin: Research Repository UCD
op_collection_id ftunivcolldublin
language English
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.
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. European Commission - Seventh Framework Programme (FP7)
format Article in Journal/Newspaper
author Eibl, Eva P. S.
Lokmer, Ivan
Bean, Christopher J.
author_facet Eibl, Eva P. S.
Lokmer, Ivan
Bean, Christopher J.
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
publisher Elsevier
publishDate 2015
url http://hdl.handle.net/10197/7005
https://doi.org/10.1016/j.jvolgeores.2015.08.002
genre Hekla
Iceland
genre_facet Hekla
Iceland
op_relation Journal of Volcanology and Geothermal Research
http://hdl.handle.net/10197/7005
304
108
117
doi:10.1016/j.jvolgeores.2015.08.002
op_rights This is the author’s version of a work that was accepted for publication in Journal of Volcanology and Geothermal Research. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Journal of Volcanology and Geothermal Research (VOL 304, ISSUE 2015, (2015)) DOI:10.1016/j.jvolgeores.2015.08.002
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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