EGU2020-10156
https://doi.org/10.5194/egusphere-egu2020-10156
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Location of Stromboli volcano July 2019 paroxysm event based on long-range infrasound detections in several IMS stations

Sandro Matos1, Nicolau Wallenstein1, Emanuele Marchetti2, and Maurizio Ripepe2
Sandro Matos et al.
  • 1Instituto de Investigação em Vulcanologia e Avaliação de Riscos (IVAR), Universidade dos Açores, Ponta Delgada, Portugal (sandro.b.matos@azores.gov.pt)
  • 2Dipartimento di Scienze della Terra, Università di Firenze, Firenze, Italy (emanuele.marchetti@unifi.it)

Stromboli is one of the most active volcanoes on Earth with a continuous explosive activity and persistent degassing since at least 3-7 AD (Rossi et al., 2000). Being an open conduit volcano, its spectacular basaltic explosions interspersed by lava fountains occurring every ≈10 minutes (Ripepe et al., 2002) make it probably the world's best-know and best-monitored volcano.

On 3rd July 2019 at the 14:45:43 UTC a paroxysmal explosion occurred with an ash column that rose almost 5 km above the volcano. This very strong explosive event was detected in several IMS infrasound stations, including IS42, located in the Azores islands in the middle of the North-Atlantic, at a distance of about 3,700 km.

We present the long-range infrasound detections that allowed us to locate the source based only in infrasound with an estimated error of less than 55 km from the ground truth event.

Keywords: Stromboli volcano, paroxysm, infrasound, IMS, IS42

How to cite: Matos, S., Wallenstein, N., Marchetti, E., and Ripepe, M.: Location of Stromboli volcano July 2019 paroxysm event based on long-range infrasound detections in several IMS stations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10156, https://doi.org/10.5194/egusphere-egu2020-10156, 2020

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