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dc.contributor.authorBarrière, J.
dc.contributor.authorOth, A.
dc.contributor.authord’Oreye, N.
dc.contributor.authorSubira, J.
dc.contributor.authorSmittarello, D.
dc.contributor.authorBrenot, H.
dc.contributor.authorTheys, N.
dc.contributor.authorSmets, B.
dc.date2023
dc.date.accessioned2023-09-19T10:51:37Z
dc.date.available2023-09-19T10:51:37Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/11068
dc.descriptionDuring eruptions, volcanoes produce air-pressure waves inaudible for the human ear called infrasound, which are very helpful for detecting early signs of magma at the surface. Compared to violent ash-rich explosions, recording more discrete atmospheric disturbances from effusive eruptions remains a practical challenge depending on the distance to the source. At Nyiragongo volcano (D.R. Congo), towering above a 1-million urban area, we analyzed local infrasonic records between January 2018 and April 2022. An acoustic signature from this open-vent volcano is detected up to the volcano observatory facilities in Goma city center about 17 km from its crater. We compared infrasound signals with space-based observations of the intra-crater activity (SO2 emissions, thermal anomalies, crater depth/radius). We thus obtain a comprehensive picture of Nyiragongo's eruptive activity during this period, encompassing the drainage of its lava lake during its third known flank eruption on 22 May 2021.
dc.languageeng
dc.titleLocal Infrasound Monitoring of Lava Eruptions at Nyiragongo Volcano (D.R. Congo) Using Urban and Near-Source Stations
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeinfrasound
dc.subject.freevolcano
dc.subject.freeopen-vent
dc.subject.freeNyiragongo
dc.subject.freelava lake
dc.source.titleGeophysical Research Letters
dc.source.volume50
dc.source.issue18
dc.source.pagee2023GL104664
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/2023GL104664
dc.identifier.scopus


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