Item talk:Q253305
From geokb
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"name": "Did ice-charging generate volcanic lightning during the 2016\u20132017 eruption of Bogoslof volcano, Alaska?",
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"abstract": "The 2016\u20132017 shallow submarine eruption of Bogoslof volcano in Alaska injected plumes of ash and seawater to maximum heights of ~\u200912\u00a0km. More than 4550 volcanic lightning strokes were detected by the World Wide Lightning Location Network (WWLLN) and Vaisala\u2019s Global Lightning Dataset (GLD360) over 9\u00a0months. Lightning assisted monitoring efforts by confirming ash-producing explosions in near-real time, but only 32 out of the 70 explosive events produced detectable lightning. What led to electrical activity within some of the volcanic plumes, but not others? And why did the lightning intensity wax and wane over the lifetime of individual explosions? We address these questions using multiparametric observations from ground-based lightning sensors, satellite imagery, photographs, acoustic signals, and 1D plume modeling. Detailed time-series of monitoring data show that the plumes did not produce detectable lightning until they rose higher than the atmospheric freezing level (approximated by \u2212\u200920\u00a0\u00b0C temperatures). For example, on 28 May 2017 (event 40), the delayed onset of lightning coincides with modeled ice formation in upper levels of the plume. Model results suggest that microphysical conditions inside the plume rivaled those of severe thunderstorms, with liquid water contents >\u20095\u00a0g\u00a0m\u22123\u00a0and vigorous updrafts >\u200940\u00a0m\u00a0s\u22121\u00a0in the mixed-phase region where liquid water and ice coexist. Based on these findings, we infer that \u2018thunderstorm-style\u2019 collisional ice-charging catalyzed the volcanic lightning. However, charge mechanisms likely operated on a continuum, with silicate collisions dominating\u00a0electrification\u00a0in the near-vent region, and ice charging taking over in the upper-level plumes. A key implication of this study is that lightning during the Bogoslof eruption provided a reliable indicator of sustained, ash-rich plumes (and associated hazards) above the atmospheric freezing level.",
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