Short-Term Forecasting and Detection of Explosions During the 2016–2017 Eruption of Bogoslof Volcano, Alaska

We describe a multidisciplinary approach to forecast, rapidly detect, and characterize explosive events during the 2016–2017 eruption of Bogoslof volcano, a back-arc shallow submarine volcano in Alaska’s Aleutian arc. The eruptive sequence began in December 2016 and included about 70 discrete explos...

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Main Authors: Michelle L. Coombs, Aaron G. Wech, Matthew M. Haney, John J. Lyons, David J. Schneider, Hans F. Schwaiger, Kristi L. Wallace, David Fee, Jeff T. Freymueller, Janet R. Schaefer, Gabrielle Tepp
Format: Article
Language:English
Published: Frontiers Media S.A. 2018-09-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/feart.2018.00122/full
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author Michelle L. Coombs
Aaron G. Wech
Matthew M. Haney
John J. Lyons
David J. Schneider
Hans F. Schwaiger
Kristi L. Wallace
David Fee
Jeff T. Freymueller
Janet R. Schaefer
Gabrielle Tepp
author_facet Michelle L. Coombs
Aaron G. Wech
Matthew M. Haney
John J. Lyons
David J. Schneider
Hans F. Schwaiger
Kristi L. Wallace
David Fee
Jeff T. Freymueller
Janet R. Schaefer
Gabrielle Tepp
author_sort Michelle L. Coombs
collection DOAJ
description We describe a multidisciplinary approach to forecast, rapidly detect, and characterize explosive events during the 2016–2017 eruption of Bogoslof volcano, a back-arc shallow submarine volcano in Alaska’s Aleutian arc. The eruptive sequence began in December 2016 and included about 70 discrete explosive events. Because the volcano has no local monitoring stations, we used distant stations on the nearest volcanoes, Okmok (54 km) and Makushin (72 km), combined with regional infrasound sensors and lightning detection from the Worldwide Lightning Location Network (WWLLN). Pre-eruptive seismicity was detected for 12 events during the first half of the eruption; for all other events co-eruptive signals allowed for detection only. Monitoring of activity used a combination of scheduled checks combined with automated alarms. Alarms triggered on real-time data included real-time seismic amplitude measurement (RSAM); infrasound from several arrays, the closest being on Okmok; and lightning strokes detected from WWLLN within a 20-km radius of the volcano. During periods of unrest, a multidisciplinary response team of four people fulfilled specific roles to evaluate geophysical and remote-sensing data, run event-specific ash-cloud dispersion models, ensure interagency coordination, and develop and distribute of formalized warning products. Using this approach, for events that produced ash clouds ≥7.5 km above sea level, Alaska Volcano Observatory (AVO) called emergency response partners 15 min, and issued written notices 30 min, after event onset (mean times). Factors that affect timeliness of written warnings include event size and number of data streams available; bigger events and more data both decrease uncertainty and allow for faster warnings. In remote areas where airborne ash is the primary hazard, the approach used at Bogoslof is an effective strategy for hazard mitigation.
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spelling doaj.art-fa13067347a84fb485a9d3d8027c36ea2022-12-21T18:55:11ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632018-09-01610.3389/feart.2018.00122376183Short-Term Forecasting and Detection of Explosions During the 2016–2017 Eruption of Bogoslof Volcano, AlaskaMichelle L. Coombs0Aaron G. Wech1Matthew M. Haney2John J. Lyons3David J. Schneider4Hans F. Schwaiger5Kristi L. Wallace6David Fee7Jeff T. Freymueller8Janet R. Schaefer9Gabrielle Tepp10Alaska Volcano Observatory, Volcano Science Center, United States Geological Survey, Anchorage, AK, United StatesAlaska Volcano Observatory, Volcano Science Center, United States Geological Survey, Anchorage, AK, United StatesAlaska Volcano Observatory, Volcano Science Center, United States Geological Survey, Anchorage, AK, United StatesAlaska Volcano Observatory, Volcano Science Center, United States Geological Survey, Anchorage, AK, United StatesAlaska Volcano Observatory, Volcano Science Center, United States Geological Survey, Anchorage, AK, United StatesAlaska Volcano Observatory, Volcano Science Center, United States Geological Survey, Anchorage, AK, United StatesAlaska Volcano Observatory, Volcano Science Center, United States Geological Survey, Anchorage, AK, United StatesAlaska Volcano Observatory, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, United StatesAlaska Volcano Observatory, Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, United StatesAlaska Volcano Observatory, Alaska Division of Geological and Geophysical Surveys, Fairbanks, AK, United StatesAlaska Volcano Observatory, Volcano Science Center, United States Geological Survey, Anchorage, AK, United StatesWe describe a multidisciplinary approach to forecast, rapidly detect, and characterize explosive events during the 2016–2017 eruption of Bogoslof volcano, a back-arc shallow submarine volcano in Alaska’s Aleutian arc. The eruptive sequence began in December 2016 and included about 70 discrete explosive events. Because the volcano has no local monitoring stations, we used distant stations on the nearest volcanoes, Okmok (54 km) and Makushin (72 km), combined with regional infrasound sensors and lightning detection from the Worldwide Lightning Location Network (WWLLN). Pre-eruptive seismicity was detected for 12 events during the first half of the eruption; for all other events co-eruptive signals allowed for detection only. Monitoring of activity used a combination of scheduled checks combined with automated alarms. Alarms triggered on real-time data included real-time seismic amplitude measurement (RSAM); infrasound from several arrays, the closest being on Okmok; and lightning strokes detected from WWLLN within a 20-km radius of the volcano. During periods of unrest, a multidisciplinary response team of four people fulfilled specific roles to evaluate geophysical and remote-sensing data, run event-specific ash-cloud dispersion models, ensure interagency coordination, and develop and distribute of formalized warning products. Using this approach, for events that produced ash clouds ≥7.5 km above sea level, Alaska Volcano Observatory (AVO) called emergency response partners 15 min, and issued written notices 30 min, after event onset (mean times). Factors that affect timeliness of written warnings include event size and number of data streams available; bigger events and more data both decrease uncertainty and allow for faster warnings. In remote areas where airborne ash is the primary hazard, the approach used at Bogoslof is an effective strategy for hazard mitigation.https://www.frontiersin.org/article/10.3389/feart.2018.00122/fulleruption forecastingAlaskavolcano monitoringBogoslofvolcanic infrasoundvolcanic lightning
spellingShingle Michelle L. Coombs
Aaron G. Wech
Matthew M. Haney
John J. Lyons
David J. Schneider
Hans F. Schwaiger
Kristi L. Wallace
David Fee
Jeff T. Freymueller
Janet R. Schaefer
Gabrielle Tepp
Short-Term Forecasting and Detection of Explosions During the 2016–2017 Eruption of Bogoslof Volcano, Alaska
Frontiers in Earth Science
eruption forecasting
Alaska
volcano monitoring
Bogoslof
volcanic infrasound
volcanic lightning
title Short-Term Forecasting and Detection of Explosions During the 2016–2017 Eruption of Bogoslof Volcano, Alaska
title_full Short-Term Forecasting and Detection of Explosions During the 2016–2017 Eruption of Bogoslof Volcano, Alaska
title_fullStr Short-Term Forecasting and Detection of Explosions During the 2016–2017 Eruption of Bogoslof Volcano, Alaska
title_full_unstemmed Short-Term Forecasting and Detection of Explosions During the 2016–2017 Eruption of Bogoslof Volcano, Alaska
title_short Short-Term Forecasting and Detection of Explosions During the 2016–2017 Eruption of Bogoslof Volcano, Alaska
title_sort short term forecasting and detection of explosions during the 2016 2017 eruption of bogoslof volcano alaska
topic eruption forecasting
Alaska
volcano monitoring
Bogoslof
volcanic infrasound
volcanic lightning
url https://www.frontiersin.org/article/10.3389/feart.2018.00122/full
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