Natural Seismic Event Analysis Based on Signal and Source Characteristics from two Experiments in Antarctica

This study presents geophysical data from two passive seismic measurements conducted at two different sites in Antarctica. We analyzed the signals mainly in the frequency domain through the multitaper method to extract some spectral characteristics of the signals that would have been out of reach th...

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Published inAnais da Academia Brasileira de Ciências Vol. 96; no. suppl 2; p. e20230752
Main Authors Travassos, Jandyr DE Menezes, Pedroso, Sebastião Guilherme, Neves, Christian Ricardo Silva DAS, Gomes, Ellen DE Nazaré Souza
Format Journal Article
LanguageEnglish
Portuguese
Published Brazil Academia Brasileira de Ciências 01.01.2024
Subjects
Antarctic Regions
anthropogenic sources
beamforming
calving event
Environmental Monitoring - methods
Ice Cover
MULTIDISCIPLINARY SCIENCES
multitaper method
Passive seismic
Wind
Antarctic Regions
calving event
anthropogenic sources
beamforming
multitaper method
Passive seismic
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Summary:This study presents geophysical data from two passive seismic measurements conducted at two different sites in Antarctica. We analyzed the signals mainly in the frequency domain through the multitaper method to extract some spectral characteristics of the signals that would have been out of reach through the usual FFT approach. The power spectral density of the signals carries information about the processes that generated them, allowing its correlation with their source origin and type, either natural or anthropogenic. We deal with three different source types: calving, wind, and anthropogenic origins. The former is closely related to glacier dynamics, being modulated by the prevailing atmospheric processes. At both locations the wind noise is prevalent, complicating the analysis of other events like calving. We have used data classification, estimation of the source azimuth, and seismic apparent velocity to demonstrate the viability of using geophysical methods to study glacier elastic parameters and dynamics. Moreover, the calving rate can yield a wider and more independent understanding of glacier hydrodynamics and may help to estimate the future response of the polar areas to a changing environment.
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ISSN:0001-3765
1678-2690
1678-2690
DOI:10.1590/0001-3765202420230752