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The concept of flux describes how much of something goes through a given area. More formally, it is the dot product of a vector field within an area. For a better understanding, consider an open rectangular surface with a small area that is placed in a uniform electric field. The larger the area, the more field lines go through it and, hence, the greater the flux; similarly, the stronger the electric field (represented by a greater density of lines), the greater the flux. On the other hand, if...
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Method for Recording Broadband High Resolution Emission Spectra of Laboratory Lightning Arcs
07:51

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Published on: August 27, 2019

Electrical activity during the 2006 Mount St. Augustine volcanic eruptions.

R J Thomas1, P R Krehbiel, W Rison

  • 1Langmuir Laboratory, New Mexico Tech, Socorro, NM 87801, USA. thomas@nmt.edu

Science (New York, N.Y.)
|February 27, 2007
PubMed
Summary

Volcanic eruptions can generate lightning through two distinct electrical phases: an explosive ejection of charged material and subsequent in-plume discharges. These findings shed light on volcanic electrical phenomena.

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Area of Science:

  • Geophysics
  • Atmospheric science
  • Volcanology

Background:

  • Volcanic eruptions are complex phenomena with poorly understood electrical aspects.
  • Lightning generation within volcanic plumes has been observed but not fully characterized.

Purpose of the Study:

  • To investigate the electrical activity associated with volcanic eruptions.
  • To differentiate the modes and characteristics of lightning during an eruption.

Main Methods:

  • Utilized radio frequency time-of-arrival (RF TOA) measurements.
  • Employed interferometer measurements to analyze electrical discharges.
  • Observed electrical activity during a Mount St. Augustine eruption.

Main Results:

  • Identified two distinct phases of electrical activity during the eruption.
  • Phase 1: Explosive ejection of positively charged volcanic ejecta with disorganized discharges and simple lightning.
  • Phase 2: Conventional lightning within the volcanic plume, with delayed onset and downwind propagation, suggesting in situ charging.

Conclusions:

  • Volcanic eruptions exhibit complex electrical behavior with at least two distinct modes.
  • The electrical activity shares similarities with thunderstorm electrification processes.
  • Further research is needed to fully understand in situ charging mechanisms in volcanic plumes.