2022
DOI: 10.1785/0220220240
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The Hunga Tonga–Hunga Ha’apai Eruption of 15 January 2022: Observations on the International Monitoring System (IMS) Hydroacoustic Stations and Synergy with Seismic and Infrasound Sensors

Abstract: Examination of the International Monitoring System (IMS) hydroacoustic data recorded during the 15 January 2022 eruption of the Hunga Tonga–Hunga Ha’apai (HTHH) volcano shows that the in-water hydroacoustic sensors recorded a long-duration (40 min) activity starting before and ending after the paroxysmal HTHH eruption at about 4:15 UTC. The main eruption at 4:15 UTC simultaneously generated low-frequency [0.001–0.05] Hz seismic body waves and large infrasound waves in the atmosphere, as well as a tsunami. The … Show more

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Cited by 8 publications
(5 citation statements)
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“…S7) are observed in both results. These signals produced infrasound and hydroacoustic phases ( 8 , 41 ) and also match the timing of volcanic activity as observed in satellite imagery ( 42 ), suggesting that this was a secondary explosive stage of the 15 January 2022 eruptive period. The events identified as E 1 and E 3 are associated with widely recorded infrasound events ( 8 , 41 ), whereas E 2 is not.…”
Section: Resultssupporting
confidence: 70%
See 2 more Smart Citations
“…S7) are observed in both results. These signals produced infrasound and hydroacoustic phases ( 8 , 41 ) and also match the timing of volcanic activity as observed in satellite imagery ( 42 ), suggesting that this was a secondary explosive stage of the 15 January 2022 eruptive period. The events identified as E 1 and E 3 are associated with widely recorded infrasound events ( 8 , 41 ), whereas E 2 is not.…”
Section: Resultssupporting
confidence: 70%
“…These signals produced infrasound and hydroacoustic phases ( 8 , 41 ) and also match the timing of volcanic activity as observed in satellite imagery ( 42 ), suggesting that this was a secondary explosive stage of the 15 January 2022 eruptive period. The events identified as E 1 and E 3 are associated with widely recorded infrasound events ( 8 , 41 ), whereas E 2 is not. We believe that the reason E 2 is not associated with an infrasound arrival is that it only began ~200 s after E 1 , making it difficult to isolate in the dispersed infrasound signal and coda of the earlier event, whereas our high-resolution seismic data deconvolution and inversion clearly resolve the signals in E 2 .…”
Section: Resultssupporting
confidence: 70%
See 1 more Smart Citation
“…In space, the loci of MFCI explosions need not necessarily be the same as the sites where eruptive products vented. Hence, the timing, spatial extent, and strength of the eruptive events deduced from satellite and ground observations ( 8 , 15 , 16 , 39 42 ) may not jive with those same features of explosive events extracted from tsunami data. Our goal is to develop a plausible time history of explosive events that explain 118 observed wave runup measurements and the two available tide gauge records in Nuku’alofa, as illuminated by tsunami simulation.…”
Section: Resultsmentioning
confidence: 99%
“…Curious that the largest explosive event of the sequence falls nearly one-half hour after the largest eruptive events, which occurred between 4:15 and 4:30 UTC ( 9 , 12 , 13 , 37 ). Curious too is that the largest explosive event of the sequence has a negligible expression in the global teleseismic records ( 12 , 13 , 41 , 42 ). Perhaps Blast 5 was not the same phreatomagmatic explosion-driven detonation as Blasts 3 and 4?…”
Section: Discussionmentioning
confidence: 99%