Articles | Volume 16, issue 3
Nat. Hazards Earth Syst. Sci., 16, 871–874, 2016
https://doi.org/10.5194/nhess-16-871-2016
Nat. Hazards Earth Syst. Sci., 16, 871–874, 2016
https://doi.org/10.5194/nhess-16-871-2016

Research article 29 Mar 2016

Research article | 29 Mar 2016

Lightning and electrical activity during the Shiveluch volcano eruption on 16 November 2014

Boris M. Shevtsov et al.

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Features of the Earth surface deformations in the Kamchatka peninsula and their relation to geoacoustic emission
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Solid Earth, 5, 1293–1300, https://doi.org/10.5194/se-5-1293-2014,https://doi.org/10.5194/se-5-1293-2014, 2014

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Cited articles

Ewert, J. W., Holzworth, R. H., and Diefenbach, A. K.: Global detection of explosive volcanic eruptions with the World Wide Lightning Location Network (WWLLN) and application to aviation safety, Invited paper, American Geophysical Union, Fall Meeting, December 2010, San Francisco, abstract #AE31A-04, 2010.
Hutchins, M. L., Holzworth, R. H., Rodger, C. J., and Brundell, J. B.: Far field power of lightning strokes as measured by the World Wide Lightning Location Network, J. Tech. (AMS), 29, 1102–1110, 2012.
James, M. R., Lane, S. J., and Gilbert, J. S.: Volcanic plume monitoring using atmospheric electrical potential gradients, J. Geol. Soc. Lond., 155, 587–590, 1998.
James, M. R., Lane, S. J., and Gilbert, J. S.: Density, construction, and drag coefficient of electrostatic volcanic ash aggregates, J. Geophys. Res., 108, 2435, 2003.
Lane, S. J., James, M. R., and Gilbert, J. S.: Electrostatic phenomena in volcanic eruptions, J. Phys., 301, 012004, https://doi.org/10.1088/1742-6596/301/1/012004, 2011.
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Short summary
The Kamchatka volcano group is located near populated areas and international air routes. Due to this, explosive eruptions are a serious threat to their security. To decrease the risks, effective systems for remote detection of eruptions are necessary. WWLLN resolution is enough for the remote sensing of the volcano lightning activity in the early stage of ash cloud formation a few minutes after the eruption when electrification proceeds the most intensively.
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