2018年12月西西里岛埃特纳火山近期活动期间电离层低层湍流变化

M. Contadakis, D. Arabelos, E. Scordilis
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摘要

本文从埃特纳火山活动前和活动期间的TEC观测资料,对电离层湍流进行了研究。埃特纳火山位于西西里岛东海岸附近。埃特纳火山的最后一次喷发发生在2018年12月24日,两天后(12月26日,UTC时间02:19),火山东南方向约15公里处发生了5.0级地震,对附近的卡塔尼亚市造成了破坏。在埃特纳火山活动的背景下,我们的调查结果表明,电离层湍流带含量的高频极限随着火山喷发时间的增加而增加,同时随着距离火山的距离而减少。我们的结论是,通过声波或重力波的LAIC机制可以解释这种现象,因为它发生在地震活动的情况下。我们的观测表明,火山喷发对电离层湍流带含量的影响在距离大于1000km(最多)时是不显著的,这是我们在研究电离层湍流与地震前兆研究的关系时必须考虑的一个事实。
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Lower Ionospheric Turbulence Variations During the Recent Activity of Etna’s Volcano, Sicily, in December 2018
In this paper, we present an investigation on the ionospheric turbulence from TEC observations before and during the recent activity of Etna’s Volcano. Mount Etna is located close to the eastern coast of Sicily. The last eruption of Etna volcano took place on 24 December 2018 while two days later (26 December, 02:19 UTC) an earthquake of M=5.0 occurred ~15 km to the ESE of the volcano, causing damage to the nearby city of Catania. The results of our investigation, on the occasion of the Etna’s Volcanic activity, indicate that the high-frequency limit fo  of the ionospheric turbulence band content, is increasing with time to the volcano eruption while, at the same time, fo isdecreasing with distance from the volcano. We conclude that the LAIC mechanism through acoustic or gravity waves could explain this phenomenology, as it has happened in cases of earthquake activity. Our observations indicate that the effect of volcanic eruption on the band content of the ionospheric turbulence is insignificant at distances greater than 1000km (at the most), a fact that we must consider in our research on Ionospheric turbulence in relation to earthquake precursors research.
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