Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons
Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Matoza, Robin S [verfasserIn] |
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| Format: |
Artikel |
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| Erschienen: |
2017 |
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| Rechteinformationen: |
Nutzungsrecht: © Acoustical Society of America |
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| Systematik: |
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| Übergeordnetes Werk: |
Enthalten in: The journal of the Acoustical Society of America - Melville, NY : AIP, 1929, 141(2017), 5, Seite 3566-3566 |
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| Übergeordnetes Werk: |
volume:141 ; year:2017 ; number:5 ; pages:3566-3566 |
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| DOI / URN: |
10.1121/1.4987573 |
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| 245 | 1 | 0 | |a Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons |
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| 520 | |a Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging because infrasound sensors are usually deployed on the ground surface. We attempt to overcome this observational limitation using a novel deployment of infrasound sensors on tethered balloons in tandem with a suite of dense ground-based seismo-acoustic, geochemical, and eruption imaging instrumentation. We conducted a collaborative multiparametric field experiment at the active Yasur volcano, Tanna Island, Vanuatu, from 26 July to 2 August 2016. Our observations include data from a temporary network of 11 broadband seismometers, 6 single infrasonic microphones, 7 small-aperture 3-element infrasound arrays, 2 infrasound sensor packages on tethered balloons, an FTIR, a FLIR, 2 scanning Flyspecs, and various visual imaging data; scoria and ash samples were collected for petrological analyses. This unprecedented dataset should provide a unique window into processes operating in the shallow magma plumbing system and their relation to subaerial eruption dynamics. | ||
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10.1121/1.4987573 doi PQ20170901 (DE-627)OLC1996120042 (DE-599)GBVOLC1996120042 (PRQ)scitation_primary_10_1121_1_49875730 (KEY)0112299120170000141000503566seismoacousticwavefieldofstrombolianexplosionsatya DE-627 ger DE-627 rakwb 530 DE-600 LING fid EQ 1000: AVZ rvk 33.12 bkl 50.36 bkl Matoza, Robin S verfasserin aut Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging because infrasound sensors are usually deployed on the ground surface. We attempt to overcome this observational limitation using a novel deployment of infrasound sensors on tethered balloons in tandem with a suite of dense ground-based seismo-acoustic, geochemical, and eruption imaging instrumentation. We conducted a collaborative multiparametric field experiment at the active Yasur volcano, Tanna Island, Vanuatu, from 26 July to 2 August 2016. Our observations include data from a temporary network of 11 broadband seismometers, 6 single infrasonic microphones, 7 small-aperture 3-element infrasound arrays, 2 infrasound sensor packages on tethered balloons, an FTIR, a FLIR, 2 scanning Flyspecs, and various visual imaging data; scoria and ash samples were collected for petrological analyses. This unprecedented dataset should provide a unique window into processes operating in the shallow magma plumbing system and their relation to subaerial eruption dynamics. Nutzungsrecht: © Acoustical Society of America Jolly, Arthur oth Fee, David oth Johnson, Richard oth Chouet, Bernard oth Dawson, Phillip oth Kilgour, Geoff oth Christenson, Bruce oth Garaebiti, Esline oth Iezzi, Alex oth Austin, Allison oth Kennedy, Ben oth Fitzgerald, Rebecca oth Key, Nick oth Enthalten in The journal of the Acoustical Society of America Melville, NY : AIP, 1929 141(2017), 5, Seite 3566-3566 (DE-627)129550264 (DE-600)219231-7 (DE-576)015003663 0001-4966 nnns volume:141 year:2017 number:5 pages:3566-3566 http://dx.doi.org/10.1121/1.4987573 Volltext http://dx.doi.org/10.1121/1.4987573 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-MUS GBV_ILN_59 GBV_ILN_60 GBV_ILN_70 GBV_ILN_120 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2006 GBV_ILN_2011 GBV_ILN_2027 GBV_ILN_2045 GBV_ILN_2192 GBV_ILN_2256 GBV_ILN_4219 GBV_ILN_4315 GBV_ILN_4319 GBV_ILN_4700 EQ 1000: 33.12 AVZ 50.36 AVZ AR 141 2017 5 3566-3566 |
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10.1121/1.4987573 doi PQ20170901 (DE-627)OLC1996120042 (DE-599)GBVOLC1996120042 (PRQ)scitation_primary_10_1121_1_49875730 (KEY)0112299120170000141000503566seismoacousticwavefieldofstrombolianexplosionsatya DE-627 ger DE-627 rakwb 530 DE-600 LING fid EQ 1000: AVZ rvk 33.12 bkl 50.36 bkl Matoza, Robin S verfasserin aut Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging because infrasound sensors are usually deployed on the ground surface. We attempt to overcome this observational limitation using a novel deployment of infrasound sensors on tethered balloons in tandem with a suite of dense ground-based seismo-acoustic, geochemical, and eruption imaging instrumentation. We conducted a collaborative multiparametric field experiment at the active Yasur volcano, Tanna Island, Vanuatu, from 26 July to 2 August 2016. Our observations include data from a temporary network of 11 broadband seismometers, 6 single infrasonic microphones, 7 small-aperture 3-element infrasound arrays, 2 infrasound sensor packages on tethered balloons, an FTIR, a FLIR, 2 scanning Flyspecs, and various visual imaging data; scoria and ash samples were collected for petrological analyses. This unprecedented dataset should provide a unique window into processes operating in the shallow magma plumbing system and their relation to subaerial eruption dynamics. Nutzungsrecht: © Acoustical Society of America Jolly, Arthur oth Fee, David oth Johnson, Richard oth Chouet, Bernard oth Dawson, Phillip oth Kilgour, Geoff oth Christenson, Bruce oth Garaebiti, Esline oth Iezzi, Alex oth Austin, Allison oth Kennedy, Ben oth Fitzgerald, Rebecca oth Key, Nick oth Enthalten in The journal of the Acoustical Society of America Melville, NY : AIP, 1929 141(2017), 5, Seite 3566-3566 (DE-627)129550264 (DE-600)219231-7 (DE-576)015003663 0001-4966 nnns volume:141 year:2017 number:5 pages:3566-3566 http://dx.doi.org/10.1121/1.4987573 Volltext http://dx.doi.org/10.1121/1.4987573 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-MUS GBV_ILN_59 GBV_ILN_60 GBV_ILN_70 GBV_ILN_120 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2006 GBV_ILN_2011 GBV_ILN_2027 GBV_ILN_2045 GBV_ILN_2192 GBV_ILN_2256 GBV_ILN_4219 GBV_ILN_4315 GBV_ILN_4319 GBV_ILN_4700 EQ 1000: 33.12 AVZ 50.36 AVZ AR 141 2017 5 3566-3566 |
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10.1121/1.4987573 doi PQ20170901 (DE-627)OLC1996120042 (DE-599)GBVOLC1996120042 (PRQ)scitation_primary_10_1121_1_49875730 (KEY)0112299120170000141000503566seismoacousticwavefieldofstrombolianexplosionsatya DE-627 ger DE-627 rakwb 530 DE-600 LING fid EQ 1000: AVZ rvk 33.12 bkl 50.36 bkl Matoza, Robin S verfasserin aut Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging because infrasound sensors are usually deployed on the ground surface. We attempt to overcome this observational limitation using a novel deployment of infrasound sensors on tethered balloons in tandem with a suite of dense ground-based seismo-acoustic, geochemical, and eruption imaging instrumentation. We conducted a collaborative multiparametric field experiment at the active Yasur volcano, Tanna Island, Vanuatu, from 26 July to 2 August 2016. Our observations include data from a temporary network of 11 broadband seismometers, 6 single infrasonic microphones, 7 small-aperture 3-element infrasound arrays, 2 infrasound sensor packages on tethered balloons, an FTIR, a FLIR, 2 scanning Flyspecs, and various visual imaging data; scoria and ash samples were collected for petrological analyses. This unprecedented dataset should provide a unique window into processes operating in the shallow magma plumbing system and their relation to subaerial eruption dynamics. Nutzungsrecht: © Acoustical Society of America Jolly, Arthur oth Fee, David oth Johnson, Richard oth Chouet, Bernard oth Dawson, Phillip oth Kilgour, Geoff oth Christenson, Bruce oth Garaebiti, Esline oth Iezzi, Alex oth Austin, Allison oth Kennedy, Ben oth Fitzgerald, Rebecca oth Key, Nick oth Enthalten in The journal of the Acoustical Society of America Melville, NY : AIP, 1929 141(2017), 5, Seite 3566-3566 (DE-627)129550264 (DE-600)219231-7 (DE-576)015003663 0001-4966 nnns volume:141 year:2017 number:5 pages:3566-3566 http://dx.doi.org/10.1121/1.4987573 Volltext http://dx.doi.org/10.1121/1.4987573 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-MUS GBV_ILN_59 GBV_ILN_60 GBV_ILN_70 GBV_ILN_120 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2006 GBV_ILN_2011 GBV_ILN_2027 GBV_ILN_2045 GBV_ILN_2192 GBV_ILN_2256 GBV_ILN_4219 GBV_ILN_4315 GBV_ILN_4319 GBV_ILN_4700 EQ 1000: 33.12 AVZ 50.36 AVZ AR 141 2017 5 3566-3566 |
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10.1121/1.4987573 doi PQ20170901 (DE-627)OLC1996120042 (DE-599)GBVOLC1996120042 (PRQ)scitation_primary_10_1121_1_49875730 (KEY)0112299120170000141000503566seismoacousticwavefieldofstrombolianexplosionsatya DE-627 ger DE-627 rakwb 530 DE-600 LING fid EQ 1000: AVZ rvk 33.12 bkl 50.36 bkl Matoza, Robin S verfasserin aut Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging because infrasound sensors are usually deployed on the ground surface. We attempt to overcome this observational limitation using a novel deployment of infrasound sensors on tethered balloons in tandem with a suite of dense ground-based seismo-acoustic, geochemical, and eruption imaging instrumentation. We conducted a collaborative multiparametric field experiment at the active Yasur volcano, Tanna Island, Vanuatu, from 26 July to 2 August 2016. Our observations include data from a temporary network of 11 broadband seismometers, 6 single infrasonic microphones, 7 small-aperture 3-element infrasound arrays, 2 infrasound sensor packages on tethered balloons, an FTIR, a FLIR, 2 scanning Flyspecs, and various visual imaging data; scoria and ash samples were collected for petrological analyses. This unprecedented dataset should provide a unique window into processes operating in the shallow magma plumbing system and their relation to subaerial eruption dynamics. Nutzungsrecht: © Acoustical Society of America Jolly, Arthur oth Fee, David oth Johnson, Richard oth Chouet, Bernard oth Dawson, Phillip oth Kilgour, Geoff oth Christenson, Bruce oth Garaebiti, Esline oth Iezzi, Alex oth Austin, Allison oth Kennedy, Ben oth Fitzgerald, Rebecca oth Key, Nick oth Enthalten in The journal of the Acoustical Society of America Melville, NY : AIP, 1929 141(2017), 5, Seite 3566-3566 (DE-627)129550264 (DE-600)219231-7 (DE-576)015003663 0001-4966 nnns volume:141 year:2017 number:5 pages:3566-3566 http://dx.doi.org/10.1121/1.4987573 Volltext http://dx.doi.org/10.1121/1.4987573 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-MUS GBV_ILN_59 GBV_ILN_60 GBV_ILN_70 GBV_ILN_120 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2006 GBV_ILN_2011 GBV_ILN_2027 GBV_ILN_2045 GBV_ILN_2192 GBV_ILN_2256 GBV_ILN_4219 GBV_ILN_4315 GBV_ILN_4319 GBV_ILN_4700 EQ 1000: 33.12 AVZ 50.36 AVZ AR 141 2017 5 3566-3566 |
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10.1121/1.4987573 doi PQ20170901 (DE-627)OLC1996120042 (DE-599)GBVOLC1996120042 (PRQ)scitation_primary_10_1121_1_49875730 (KEY)0112299120170000141000503566seismoacousticwavefieldofstrombolianexplosionsatya DE-627 ger DE-627 rakwb 530 DE-600 LING fid EQ 1000: AVZ rvk 33.12 bkl 50.36 bkl Matoza, Robin S verfasserin aut Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging because infrasound sensors are usually deployed on the ground surface. We attempt to overcome this observational limitation using a novel deployment of infrasound sensors on tethered balloons in tandem with a suite of dense ground-based seismo-acoustic, geochemical, and eruption imaging instrumentation. We conducted a collaborative multiparametric field experiment at the active Yasur volcano, Tanna Island, Vanuatu, from 26 July to 2 August 2016. Our observations include data from a temporary network of 11 broadband seismometers, 6 single infrasonic microphones, 7 small-aperture 3-element infrasound arrays, 2 infrasound sensor packages on tethered balloons, an FTIR, a FLIR, 2 scanning Flyspecs, and various visual imaging data; scoria and ash samples were collected for petrological analyses. This unprecedented dataset should provide a unique window into processes operating in the shallow magma plumbing system and their relation to subaerial eruption dynamics. Nutzungsrecht: © Acoustical Society of America Jolly, Arthur oth Fee, David oth Johnson, Richard oth Chouet, Bernard oth Dawson, Phillip oth Kilgour, Geoff oth Christenson, Bruce oth Garaebiti, Esline oth Iezzi, Alex oth Austin, Allison oth Kennedy, Ben oth Fitzgerald, Rebecca oth Key, Nick oth Enthalten in The journal of the Acoustical Society of America Melville, NY : AIP, 1929 141(2017), 5, Seite 3566-3566 (DE-627)129550264 (DE-600)219231-7 (DE-576)015003663 0001-4966 nnns volume:141 year:2017 number:5 pages:3566-3566 http://dx.doi.org/10.1121/1.4987573 Volltext http://dx.doi.org/10.1121/1.4987573 GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-LING SSG-OLC-PHY SSG-OLC-MUS GBV_ILN_59 GBV_ILN_60 GBV_ILN_70 GBV_ILN_120 GBV_ILN_170 GBV_ILN_201 GBV_ILN_2006 GBV_ILN_2011 GBV_ILN_2027 GBV_ILN_2045 GBV_ILN_2192 GBV_ILN_2256 GBV_ILN_4219 GBV_ILN_4315 GBV_ILN_4319 GBV_ILN_4700 EQ 1000: 33.12 AVZ 50.36 AVZ AR 141 2017 5 3566-3566 |
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Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons |
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seismo-acoustic wavefield of strombolian explosions at yasur volcano, vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons |
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Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons |
| abstract |
Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging because infrasound sensors are usually deployed on the ground surface. We attempt to overcome this observational limitation using a novel deployment of infrasound sensors on tethered balloons in tandem with a suite of dense ground-based seismo-acoustic, geochemical, and eruption imaging instrumentation. We conducted a collaborative multiparametric field experiment at the active Yasur volcano, Tanna Island, Vanuatu, from 26 July to 2 August 2016. Our observations include data from a temporary network of 11 broadband seismometers, 6 single infrasonic microphones, 7 small-aperture 3-element infrasound arrays, 2 infrasound sensor packages on tethered balloons, an FTIR, a FLIR, 2 scanning Flyspecs, and various visual imaging data; scoria and ash samples were collected for petrological analyses. This unprecedented dataset should provide a unique window into processes operating in the shallow magma plumbing system and their relation to subaerial eruption dynamics. |
| abstractGer |
Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging because infrasound sensors are usually deployed on the ground surface. We attempt to overcome this observational limitation using a novel deployment of infrasound sensors on tethered balloons in tandem with a suite of dense ground-based seismo-acoustic, geochemical, and eruption imaging instrumentation. We conducted a collaborative multiparametric field experiment at the active Yasur volcano, Tanna Island, Vanuatu, from 26 July to 2 August 2016. Our observations include data from a temporary network of 11 broadband seismometers, 6 single infrasonic microphones, 7 small-aperture 3-element infrasound arrays, 2 infrasound sensor packages on tethered balloons, an FTIR, a FLIR, 2 scanning Flyspecs, and various visual imaging data; scoria and ash samples were collected for petrological analyses. This unprecedented dataset should provide a unique window into processes operating in the shallow magma plumbing system and their relation to subaerial eruption dynamics. |
| abstract_unstemmed |
Seismo-acoustic wavefields at volcanoes contain rich information on shallow magma transport and subaerial eruption processes and inform our understanding of how volcanoes work. Acoustic wavefields from eruptions are predicted to be directional, but sampling this wavefield directivity is challenging because infrasound sensors are usually deployed on the ground surface. We attempt to overcome this observational limitation using a novel deployment of infrasound sensors on tethered balloons in tandem with a suite of dense ground-based seismo-acoustic, geochemical, and eruption imaging instrumentation. We conducted a collaborative multiparametric field experiment at the active Yasur volcano, Tanna Island, Vanuatu, from 26 July to 2 August 2016. Our observations include data from a temporary network of 11 broadband seismometers, 6 single infrasonic microphones, 7 small-aperture 3-element infrasound arrays, 2 infrasound sensor packages on tethered balloons, an FTIR, a FLIR, 2 scanning Flyspecs, and various visual imaging data; scoria and ash samples were collected for petrological analyses. This unprecedented dataset should provide a unique window into processes operating in the shallow magma plumbing system and their relation to subaerial eruption dynamics. |
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Seismo-acoustic wavefield of strombolian explosions at Yasur volcano, Vanuatu, using a broadband seismo-acoustic network, infrasound arrays, and infrasonic sensors on tethered balloons |
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