TY - JOUR
T1 - Lightning and Electrical Activity During the Eruptions of Augustine Volcano
AU - Thomas, Ronald J.
AU - McNutt, Stephen R.
AU - Krehbiel, Paul R.
AU - Rison, William
AU - Aulich, Grayden
AU - Edens, Harald E.
AU - Tytgat, Guy
AU - Clark, Edward
PY - 2010/1/1
Y1 - 2010/1/1
N2 - Lightning and other electrical activity were measured during the 2006 eruption of Augustine Volcano. We found two phases of the activity, the explosive phase corresponding to the explosive eruptions and the plume phase. We classified the lightning into three types, vent discharges, near-vent lightning, and plume lightning. Vent discharges are small, 10 to 100 m sparks, that occur at rate as great as 10,000 s-1 at the mouth of the volcano during the energetic explosive eruptions. The vent discharges were observed six different times. Near-vent lightning appears to develop upward from the volcanic cone into the developing column during explosions. This lightning is small, in the range of 1 to 7 km, and short, 0.01 to 0.1 s. The behavior of the near-vent lightning indicates an overall positive charge in the ejecta. The plume lightning resembled intracloud thunderstorm lightning. Often it was branched, spanned more than 10 km, and lasted more than 0.5 s.
AB - Lightning and other electrical activity were measured during the 2006 eruption of Augustine Volcano. We found two phases of the activity, the explosive phase corresponding to the explosive eruptions and the plume phase. We classified the lightning into three types, vent discharges, near-vent lightning, and plume lightning. Vent discharges are small, 10 to 100 m sparks, that occur at rate as great as 10,000 s-1 at the mouth of the volcano during the energetic explosive eruptions. The vent discharges were observed six different times. Near-vent lightning appears to develop upward from the volcanic cone into the developing column during explosions. This lightning is small, in the range of 1 to 7 km, and short, 0.01 to 0.1 s. The behavior of the near-vent lightning indicates an overall positive charge in the ejecta. The plume lightning resembled intracloud thunderstorm lightning. Often it was branched, spanned more than 10 km, and lasted more than 0.5 s.
UR - https://digitalcommons.usf.edu/geo_facpub/328
UR - http://pubs.usgs.gov/pp/1769/chapters/p1769_chapter25.pdf
M3 - Article
VL - 1769
JO - U.S. Geological Survey Professional Paper
JF - U.S. Geological Survey Professional Paper
ER -