2019年6月千岛群岛Raikoke火山爆发时全球探测到的火山闪电的空间分析

IF 2.5 Q2 Earth and Planetary Sciences
Cassandra M. Smith, A. V. Van Eaton, D. Schneider, L. Mastin, R. Matoza, Kathleen F. McKee, S. Maher
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引用次数: 1

摘要

2019年6月21日至22日,俄罗斯Raikoke火山爆发,为探索火山闪电位置的空间趋势如何提供脉动喷发动力学的见解提供了机会。利用卫星衍生的羽流高度,我们研究了维萨拉全球闪电数据集(GLD360)从11个紧密间隔的爆发脉冲中探测到的闪电的发展。一维羽流模拟结果表明,最大高度在海拔9 ~ 16.5 km的喷发脉冲能够在对流层上层产生冰,这对电气化和火山闪电有不同的贡献。一个关键的发现是,闪电的位置不仅遵循这些灰羽的主要扩散方向,而且还追踪了由火山碎屑密度流产生的低层云。我们展示了伞状云的扩张与闪电发生的区域(“闪电足迹”)之间的正相关关系。这些观测结果为近乎实时地描述正在进行的火山喷发活动提供了有用的指标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatial analysis of globally detected volcanic lightning from the June 2019 eruption of Raikoke volcano, Kuril Islands
The 21–22 June 2019 eruption of Raikoke volcano, Russia, provided an opportunity to explore how spatial trends in volcanic lightning locations provide insights into pulsatory eruption dynamics. Using satellite-derived plume heights, we examine the development of lightning detected by Vaisala’s Global Lightning Dataset (GLD360) from eleven, closely spaced eruptive pulses. Results from one-dimensional plume modeling show that the eruptive pulses with maximum heights 9–16.5 km above sea level were capable of producing ice in the upper troposphere, which contributed variably to electrification and volcanic lightning. A key finding is that lightning locations not only followed the main dispersal direction of these ash plumes, but also tracked a lower-level cloud derived from pyroclastic density currents. We show a positive relationship between umbrella cloud expansion and the area over which lightning occurs (the ‘lightning footprint’). These observations suggest useful metrics to characterize ongoing eruptive activity in near real-time.
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来源期刊
Volcanica
Volcanica Earth and Planetary Sciences-Geology
CiteScore
4.40
自引率
0.00%
发文量
21
审稿时长
21 weeks
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