2017
DOI: 10.3389/feart.2017.00048
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Assimilation of Deformation Data for Eruption Forecasting: Potentiality Assessment Based on Synthetic Cases

Abstract: In monitoring active volcanoes, the magma overpressure is one of the key parameters used in forecasting volcanic eruptions. This parameter can be inferred from the ground displacements measured on the Earth's surface by applying inversion techniques. However, in most studies, the huge amount of information about the behavior of the volcano contained in the temporal evolution of the deformation signal is not fully exploited by inversion. Our work focuses on developing a strategy in order to better forecast the … Show more

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Cited by 27 publications
(29 citation statements)
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“…Seismicity, deformation and gas measurements may be used to interpret conditions in the magma plumbing system. For instance, long period earthquakes, seismic velocity changes and ‘drumbeat’ seismicity have been used to detect magmatic ascent 109 , 119 , 147 ; pre-eruptive, InSAR and tilt data were linked to the rate of pressure change and resulting explosivity of an eruption 148 , 149 ; and increases in CO 2 relative to SO 2 phases have been recorded before some explosive eruptions 150 , 151 . However, those monitoring techniques require much refinement before volcanologists can, in near real-time predict future behaviours of a given volcano.…”
Section: Forecasting Eruptive Stylementioning
confidence: 99%
“…Seismicity, deformation and gas measurements may be used to interpret conditions in the magma plumbing system. For instance, long period earthquakes, seismic velocity changes and ‘drumbeat’ seismicity have been used to detect magmatic ascent 109 , 119 , 147 ; pre-eruptive, InSAR and tilt data were linked to the rate of pressure change and resulting explosivity of an eruption 148 , 149 ; and increases in CO 2 relative to SO 2 phases have been recorded before some explosive eruptions 150 , 151 . However, those monitoring techniques require much refinement before volcanologists can, in near real-time predict future behaviours of a given volcano.…”
Section: Forecasting Eruptive Stylementioning
confidence: 99%
“…The EnKF solves the Bayesian update problem using a Monte Carlo method (Evensen, ). We follow the same strategy developed in previous studies using the EnKF method to model volcanic deformation (Figure ; Gregg & Pettijohn, ; Zhan & Gregg, ; Zhan et al, ; Bato et al, , ; Albright et al, ). The EnKF analysis updates the physical model ( A a ) by Aaitalic=bold-italicAitalic+PeHTHbold-italicPebold-italicHT+bold-italicReitalic−italic1()bold-italicDitalic−bold-italicHbold-italicAitalic, where A is a matrix containing the parameters and states of all ensemble models whose covariance matrix is P e .…”
Section: Magma Body Architecturementioning
confidence: 99%
“…The EnKF solves the Bayesian update problem using a Monte Carlo method (Evensen, 2003). We follow the same strategy developed in previous studies using the EnKF method to model volcanic deformation (Figure 3; Gregg & Pettijohn, 2015;Bato et al, 2017Bato et al, , 2018Albright et al, 2019). The EnKF analysis updates the physical model (A a ) by…”
Section: Magma Body Geometry Estimation By Data Assimilationmentioning
confidence: 99%
“…While several studies have used real geodetic data and applied variants of Kalman Filter as an optimization or statistical interpolation tool to solve problems in volcanology in the past 9 – 11 , this study is the first one to apply sequential data assimilation based on a dynamical model as proposed by ref. 12 using a real dataset recorded on a volcano.…”
Section: Introductionmentioning
confidence: 99%