Integrating puffing and explosions in a general scheme for Strombolian‐style activity

• Published in: Journal of geophysical research. Solid earth 2017-03, Vol.122 (3), p.1860-1875
• Main Authors: Gaudin, Damien, Taddeucci, Jacopo, Scarlato, Piergiorgio, Bello, Elisabetta, Ricci, Tullio, Orr, Tim, Houghton, Bruce, Harris, Andrew, Rao, Sandro, Bucci, Augusto
• Format: Article
• Language: English
• Subjects: Abundance; Algorithms; Ashes; Bombs; Ejection; Eruptions; explosion precursors; Explosions; Free surfaces; gas pocket; Gas pockets; Geophysics; high‐viscosity layer; Infrared; Mathematical models; puffing; rapid explosions; Relative abundance; Seabirds; Strombolian activity; Thickness; Vents; Viscosity; Volcanic activity; Volcanism; Volcanoes
• ISSN: 2169-9313; 2169-9356
• DOI: 10.1002/2016JB013707

Strombolian eruptions are among the most common subaerial styles of explosive volcanism worldwide. Distinctive features of each volcano lead to a correspondingly wide range of variations of magnitude and erupted products, but most papers focus on a single type of event at a single volcano. Here, in order to emphasize the common features underlying this diversity of styles, we scrutinize a database from 35 different erupting vents, including 21 thermal infrared videos from Stromboli (Italy), Etna (Italy), Yasur (Vanuatu), and Batu Tara (Indonesia), from puffing, through rapid explosions to normal explosions, with variable ejection parameters and relative abundance of gas, ash, and bombs. Using field observations and high‐speed thermal infrared videos processed by a new algorithm, we identify the distinguishing characteristics of each type of activity and how they may relate and interact. In particular, we record that ash‐poor normal explosions may be preceded and followed by the onset or the increase of the puffing activity, while ash‐rich explosions are emergent, i.e., with inflation of the free surface followed directly by emission of increasingly large gas pockets. Overall, we see that all Strombolian activities form a continuum arising from a common mechanism and are modulated by the combination of two well‐established controls: (1) the length of the bursting gas pocket with respect to the vent diameter and (2) the presence and thickness of a high‐viscosity layer in the uppermost part of the volcanic conduit. Key Points We compared thermal infrared videos of Strombolian activity from 21 vents of four volcanoes A gradual spectrum exists from puffing to normal explosions and from bomb‐ to ash‐rich explosions Gas pocket length and presence of a high‐viscosity layer jointly control vent activity