Abstract

Here, we present the first ultraviolet (UV) camera measurements of sulphur dioxide (SO2) flux from Yasur volcano, Vanuatu, for the period 6–9 July 2018. These data yield the first direct gas-measurement-derived calculations of explosion gas masses at Yasur. Yasur typically exhibits persistent passive gas release interspersed with frequent Strombolian explosions. We used compact forms of the “PiCam” Raspberry Pi UV camera system powered through solar panels to collect images. Our daily median SO2 fluxes ranged from 4 to 5.1 kg s−1, with a measurement uncertainty of −12.2% to +14.7%, including errors from the gas cell calibration drift, uncertainties in plume direction and distance, and errors from the plume velocity. This work highlights the use of particle image velocimetry (PIV) for plume velocity determination, which was preferred over the typically used cross-correlation and optical flow methods because of the ability to function over a variety of plume conditions. We calculated SO2 masses for Strombolian explosions ranging 8–81 kg (mean of 32 kg), which to our knowledge is the first budget of explosive gas masses from this target. Through the use of a simple statistical measure using the moving minimum, we estimated that passive degassing is the dominant mode of gas emission at Yasur, supplying an average of ~69% of the total gas released. Our work further highlights the utility of UV camera measurements in volcanology, and particularly the benefit of the multiple camera approach in error characterisation. This work also adds to our inventory of gas-based data, which can be used to characterise the spectrum of Strombolian activity across the globe.

Highlights

  • Strombolian volcanism is one of the more common forms of basaltic explosive activity globally, associated with the rapid ejection of hot pyroclasts from a vent in a single impulsive burst [1,2], with event frequencies ranging from seconds to minutes [3]

  • We present the first UV camera measurements at Yasur, providing gas-based estimates of explosive Strombolian gas masses, which are key to unravelling information on the spectrum of behaviours for this style of activity globally

  • SO2 Fluxes and Estimates of the Masses of Gas Emitted during Strombolian Explosions

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Summary

Introduction

Strombolian volcanism is one of the more common forms of basaltic explosive activity globally, associated with the rapid ejection of hot pyroclasts from a vent in a single impulsive burst [1,2], with event frequencies ranging from seconds to minutes [3]. Other volcanoes known to produce Strombolian activity include Etna, Italy [15,16,17]; Villarrica, Chile [18]; Arenal, Costa Rica [19,20]; Batu Tara, Indonesia [21,22]; and Shishaldin, USA [23] This style of behaviour has been related to the ascent from depth of elongated and overpressured bubbles, termed gas slugs (Taylor bubbles), which rapidly expand in length as they approach the surface [2,24,25,26]. This has led to the classification of behaviour styles, ranging from rapidly bursting slugs, which may interact with one another during ascent, through to single bursting slugs [3,31]

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