Deformation Anomalies Accompanying Tsunami Origination

Basing on the analysis of data on variations of deformations in the Earth’s crust, which were obtained with a laser strainmeter, we found that deformation anomalies (deformation jumps) occurred at the time of tsunami generation. Deformation jumps recorded by the laser strainmeter were apparently cau...

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Main Authors: Grigory Dolgikh, Stanislav Dolgikh
Format: Article
Language:English
Published: MDPI AG 2021-10-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/9/10/1144
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author Grigory Dolgikh
Stanislav Dolgikh
author_facet Grigory Dolgikh
Stanislav Dolgikh
author_sort Grigory Dolgikh
collection DOAJ
description Basing on the analysis of data on variations of deformations in the Earth’s crust, which were obtained with a laser strainmeter, we found that deformation anomalies (deformation jumps) occurred at the time of tsunami generation. Deformation jumps recorded by the laser strainmeter were apparently caused by bottom displacements, leading to tsunami formation. According to the data for the many recorded tsunamigenic earthquakes, we calculated the damping ratios of the identified deformation anomalies for three regions of the planet. We proved the obtained experimental results by applying the sine-Gordon equation, the one-kink and two-kink solutions of which allowed us to describe the observed deformation anomalies. We also formulated the direction of a theoretical deformation jump occurrence—a kink (bore)—during an underwater landslide causing a tsunami.
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spelling doaj.art-c00819ffc9474038b03b821c6d433f4f2023-11-22T18:46:16ZengMDPI AGJournal of Marine Science and Engineering2077-13122021-10-01910114410.3390/jmse9101144Deformation Anomalies Accompanying Tsunami OriginationGrigory Dolgikh0Stanislav Dolgikh1V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch Russian Academy of Sciences, 690041 Vladivostok, RussiaV.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch Russian Academy of Sciences, 690041 Vladivostok, RussiaBasing on the analysis of data on variations of deformations in the Earth’s crust, which were obtained with a laser strainmeter, we found that deformation anomalies (deformation jumps) occurred at the time of tsunami generation. Deformation jumps recorded by the laser strainmeter were apparently caused by bottom displacements, leading to tsunami formation. According to the data for the many recorded tsunamigenic earthquakes, we calculated the damping ratios of the identified deformation anomalies for three regions of the planet. We proved the obtained experimental results by applying the sine-Gordon equation, the one-kink and two-kink solutions of which allowed us to describe the observed deformation anomalies. We also formulated the direction of a theoretical deformation jump occurrence—a kink (bore)—during an underwater landslide causing a tsunami.https://www.mdpi.com/2077-1312/9/10/1144earthquaketsunamilaser strainmeterdeformation jumpsine-Gordon equationkink
spellingShingle Grigory Dolgikh
Stanislav Dolgikh
Deformation Anomalies Accompanying Tsunami Origination
Journal of Marine Science and Engineering
earthquake
tsunami
laser strainmeter
deformation jump
sine-Gordon equation
kink
title Deformation Anomalies Accompanying Tsunami Origination
title_full Deformation Anomalies Accompanying Tsunami Origination
title_fullStr Deformation Anomalies Accompanying Tsunami Origination
title_full_unstemmed Deformation Anomalies Accompanying Tsunami Origination
title_short Deformation Anomalies Accompanying Tsunami Origination
title_sort deformation anomalies accompanying tsunami origination
topic earthquake
tsunami
laser strainmeter
deformation jump
sine-Gordon equation
kink
url https://www.mdpi.com/2077-1312/9/10/1144
work_keys_str_mv AT grigorydolgikh deformationanomaliesaccompanyingtsunamiorigination
AT stanislavdolgikh deformationanomaliesaccompanyingtsunamiorigination