Constraints on eruption processes and event masses for the 2016–2017 eruption of Bogoslof volcano, Alaska, through evaluation of IASI satellite SO2 masses and complementary datasets

Taryn Lopez; Lieven Clarisse; Hans Schwaiger; Alexa R. Van Eaton; Matthew W. Loewen; David Fee; John J. Lyons; Kristi L. Wallace; Cheryl Searcy; Aaron Wech; Matthew M. Haney; David J. Schneider; Nathan Graham

doi:10.1007/s00445-019-1348-z

USGS · 70215337

Constraints on eruption processes and event masses for the 2016–2017 eruption of Bogoslof volcano, Alaska, through evaluation of IASI satellite SO2 masses and complementary datasets

Taryn Lopez·Lieven Clarisse·Hans Schwaiger·Alexa R. Van Eaton·Matthew W. Loewen·David Fee·John J. Lyons·Kristi L. Wallace·Cheryl Searcy·Aaron Wech·Matthew M. Haney·David J. Schneider·Nathan Graham

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Abstract

Bogoslof volcano, Alaska, experienced at least 70 explosive eruptions between 12 December 2016 and 31 August 2017. Due to its remote location and limited local monitoring network, this eruption was monitored and characterized primarily using remote geophysical and satellite techniques. SO 2 emissions from Bogoslof were persistently detected by the Infrared Atmospheric Sounding Interferometer (IASI) satellite sensors. Of Bogoslof’s 70 explosive events, 50% produced measurable SO 2 masses ranging from 0.1 to 21.5 kt, with a median and standard deviation of 0.7 ± 4.0 kt SO 2 , respectively. Here, we compare IASI-derived SO 2 masses from Bogoslof events to complementary geophysical datasets to provide insights into eruption source processes, namely the degree of seawater scrubbing of water-soluble SO 2 and variations in magma flux. Correlations with the number of lightning strokes and infrasound energy are expected to indicate magma-flux as a controlling process, while correlations with infrasound frequency index are expected to indicate variations in vent-water content as a controlling factor. These comparisons suggest that the measured SO 2 masses are primarily a function of eruption magnitude (degassed magma mass) and that scrubbing of SO 2 emissions by vent seawater may have exerted a minor effect on the observed SO 2 masses. SO 2 masses were combined with petrologic constraints on melt inclusion and matrix glass S concentrations to calculate degassed magma masses and volumes. The cumulative SO 2 -derived degassed magma mass and estimated volume (dense-rock equivalent) for the full Bogoslof eruption were found to be 2.8 × 10 10 kg and 9.3 × 10 6 m 3 , respectively. When individual event masses are compared against event masses calculated using an empirical plume-height method, a strong correlation is found ( R 2 = 0.83), with better than order-of-magnitude agreement in most cases. These estimates of eruption masses provide useful information on the magnitude, behavior, and associated hazards of the 2016–2017 eruption, and potentially future unrest at Bogoslof volcano.

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Source-reported bounding extent: 53.04451562644129° to 54.17529672404642° latitude; -168.255615234375° to -165.47607421874997° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Taryn Lopez, Lieven Clarisse, Hans Schwaiger, Alexa R. Van Eaton, Matthew W. Loewen, David Fee, John J. Lyons, Kristi L. Wallace, Cheryl Searcy, Aaron Wech, Matthew M. Haney, David J. Schneider, Nathan Graham. 2020-01-25. Constraints on eruption processes and event masses for the 2016–2017 eruption of Bogoslof volcano, Alaska, through evaluation of IASI satellite SO2 masses and complementary datasets. https://doi.org/10.1007/s00445-019-1348-z

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