2019
DOI: 10.3390/atmos10050267
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Joint Anomalies of High-Frequency Geoacoustic Emission and Atmospheric Electric Field by the Ground–Atmosphere Boundary in a Seismically Active Region (Kamchatka)

Abstract: The authors generalize and analyze the investigation results of joint anomalies of high-frequency geoacoustic emission and atmospheric electric field by the ground–atmosphere boundary which were detected by them in Kamchatka. These anomalies are observed as geoacoustic emission increases in kilohertz frequency range and bay-like decreases of atmospheric electric field with the sign change which occur close in time during calm weather conditions. It is the authors’ opinion that the common nature of these anomal… Show more

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Cited by 8 publications
(4 citation statements)
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References 35 publications
(49 reference statements)
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“…Kamchatka is part of the Kuril–Kamchatka island (or volcanic) arc. It is one of the most seismically active regions on the Earth, with about 30 active and potentially active volcanoes in the Kuril–Kamchatka region [ 21 , 22 , 23 ]. As a result of the eruptions of these volcanoes, millions of tons of volcanic ash are emitted into the atmosphere [ 24 ].…”
Section: Introductionmentioning
confidence: 99%
“…Kamchatka is part of the Kuril–Kamchatka island (or volcanic) arc. It is one of the most seismically active regions on the Earth, with about 30 active and potentially active volcanoes in the Kuril–Kamchatka region [ 21 , 22 , 23 ]. As a result of the eruptions of these volcanoes, millions of tons of volcanic ash are emitted into the atmosphere [ 24 ].…”
Section: Introductionmentioning
confidence: 99%
“…Marapulets and Rulenko also conducted a comprehensive analysis of joint anomalies involving high-frequency acoustic emission and the AEF at the ground-atmosphere boundary in Kamchatka. These anomalies manifested as increases in acoustic emission in the mHz frequency range and bay-like decreases in the AEF that occurred simultaneously during calm weather conditions [32].…”
Section: Wavelet Analysis Resultsmentioning
confidence: 99%
“…It was shown in [1,2] that AE intensity increases at the frequency of 25 kHz 2-3 days before strong earthquakes. According to [19,20], anomalies in the form of signal level increase appear in the frequency range of more than 6.5 kHz in the AE signals accumulated by 1 s. The results of time-frequency analysis of single AE pulses registered 1-7 days before earthquakes are presented in [21,22]. According to these results, the number of pulses of a certain frequency increases before strong earthquakes.…”
Section: Examples Of Identification Of Pre-seismic Ae Anomaliesmentioning
confidence: 99%