Volcanic eruptions observed with infrasound
Geophysical Research Letters2004Vol. 31(14)
Citations Over TimeTop 10% of 2004 papers
Abstract
Infrasonic airwaves produced by active volcanoes provide valuable insight into the eruption dynamics. Because the infrasonic pressure field may be directly associated with the flux rate of gas released at a volcanic vent, infrasound also enhances the efficacy of volcanic hazard monitoring and continuous studies of conduit processes. Here we present new results from Erebus, Fuego, and Villarrica volcanoes highlighting uses of infrasound for constraining quantitative eruption parameters, such as eruption duration, source mechanism, and explosive gas flux.
Related Papers
- → Infrasound reveals transition to oscillatory discharge regime during lava fountaining: Implication for early warning(2013)70 cited
- → Monochromatic infrasound waves observed during the 2014–2015 eruption of Aso volcano, Japan(2019)33 cited
- → Analyzing continuous infrasound from Stromboli volcano, Italy using unsupervised machine learning(2020)21 cited
- → Towards an Automatic Monitoring System of Infrasonic Events at Mt. Etna: Strategies for Source Location and Modeling(2010)19 cited
- → Multiphase Flows in Volcanic Eruption(2015)