During the last few decades, infrasound signals have been used to investigate and monitor active volcanoes during eruptive and degassing activity. Researchers estimated eruptive parameters, such as plume height, magma discharge rate and lava fountain height, from infrasound amplitude observations. Active volcanoes are characterized by pronounced topography and, during eruptive activity, the topography can change rapidly. Several studies have demonstrated how the interaction of infrasonic signals with the topography between the receiver and the source can significantly affect their propagation at local scales. While this interaction has been investigated by several authors over the past decade, the impact of changing topography on the infrasonic amplitudes has not yet been explored. In this work, the infrasonic signals accompanying 57 lava fountain paroxysms at Mount Etna (Italy) during 2021 were analyzed. In particular, the temporal and spatial variations of the infrasound amplitudes were investigated. The paroxysms took place at the South-East Crater (SEC) from 16 February to 23 October (two sequences: the first sequence began on 16 February and ended on 1 April 2021; the second sequence began on 19 May and ended on 23 October 2021). During 2021, significant changes in the topography around the SEC took place and were reconstructed in detail through unoccupied aerial system surveys. Through analysis of the observed infrasound signals and numerical simulations of the acoustic wavefield, we demonstrate that the observed spatial and temporal variation in the infrasound signals can be explained by the combined effects of changes in the location of the acoustic source and changes in the near-vent topography. This work demonstrates the importance of accurate source locations and high-resolution topographic information, particularly in the near-vent region where the topography is most likely to change rapidly. Changing topography should be considered when interpreting local infrasound observations over long time-scales.
How topographic changes influenced infrasound amplitude during Mt. Etna’s 2021 lava fountains
Iozzia A.;De Beni E.;Ganci G.;Sciotto M.;Cannata A.
2023-01-01
Abstract
During the last few decades, infrasound signals have been used to investigate and monitor active volcanoes during eruptive and degassing activity. Researchers estimated eruptive parameters, such as plume height, magma discharge rate and lava fountain height, from infrasound amplitude observations. Active volcanoes are characterized by pronounced topography and, during eruptive activity, the topography can change rapidly. Several studies have demonstrated how the interaction of infrasonic signals with the topography between the receiver and the source can significantly affect their propagation at local scales. While this interaction has been investigated by several authors over the past decade, the impact of changing topography on the infrasonic amplitudes has not yet been explored. In this work, the infrasonic signals accompanying 57 lava fountain paroxysms at Mount Etna (Italy) during 2021 were analyzed. In particular, the temporal and spatial variations of the infrasound amplitudes were investigated. The paroxysms took place at the South-East Crater (SEC) from 16 February to 23 October (two sequences: the first sequence began on 16 February and ended on 1 April 2021; the second sequence began on 19 May and ended on 23 October 2021). During 2021, significant changes in the topography around the SEC took place and were reconstructed in detail through unoccupied aerial system surveys. Through analysis of the observed infrasound signals and numerical simulations of the acoustic wavefield, we demonstrate that the observed spatial and temporal variation in the infrasound signals can be explained by the combined effects of changes in the location of the acoustic source and changes in the near-vent topography. This work demonstrates the importance of accurate source locations and high-resolution topographic information, particularly in the near-vent region where the topography is most likely to change rapidly. Changing topography should be considered when interpreting local infrasound observations over long time-scales.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
