Journal
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH
Volume 324, Issue -, Pages 118-133Publisher
ELSEVIER
DOI: 10.1016/j.jvolgeores.2016.05.011
Keywords
Volcano-seismology; Failure Forecast Method; Low frequency; Multiplets; Eruption forecasting; Soufriere Hills volcano
Categories
Funding
- NERC studentship at the University of Leeds [NE/J50001X/1]
- European Union Framework Program 7 [282759]
- NERC/ESRC project Strengthening Resilience in Volcanic Areas (STREVA) [NE/J020052/1]
- NERC [NE/J02483X/1] Funding Source: UKRI
- Natural Environment Research Council [1047141, NE/J02483X/1] Funding Source: researchfish
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Prior to many volcanic eruptions, an acceleration in seismicity has been observed, suggesting the potential for this as a forecasting tool. The Failure Forecast Method (FFM) relates an accelerating precursor to the timing of failure by an empirical power law, with failure being defined in this context as the onset of an eruption. Previous applications of the FFM have used a wide variety of accelerating time series, often generating questionable forecasts with large misfits between data and the forecast, as well as the generation of a number of different forecasts from the same data series. Here, we show an alternative approach applying the FFM in combination with a cross correlation technique which identifies seismicity from a single active source mechanism and location at depth. Isolating a single system at depth avoids additional uncertainties introduced by averaging data over a number of different accelerating phenomena, and consequently reduces the misfit between the data and the forecast. Similar seismic waveforms were identified in the precursory accelerating seismicity to dome collapses at Soufriere Hills volcano, Montserrat in June 1997, July 2003 and February 2010. These events were specifically chosen since they represent a spectrum of collapse scenarios at this volcano. The cross correlation technique generates a five-fold increase in the number of seismic events which could be identified from continuous seismic data rather than using triggered data, thus providing a more holistic understanding of the ongoing seismicity at the time. The use of similar seismicity as a forecasting tool for collapses in 1997 and 2003 greatly improved the forecasted timing of the dome collapse, as well as improving the confidence in the forecast, thereby outperforming the classical application of the FFM. We suggest that focusing on a single active seismic system at depth allows a more accurate forecast of some of the major dome collapses from the ongoing eruption at Soufriere Hills volcano, and provides a simple addition to the well-used methodology of the FFM. (C) 2016 Elsevier B.V. All rights reserved.
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