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Volcanic Tremor Extraction and Earthquake Detection Using Music Information Retrieval Algorithms

Authors
/persons/resource/zali

Zali,  Zahra
2.6 Seismic Hazard and Risk Dynamics, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Ohrnberger,  Matthias
External Organizations;

Scherbaum,  Frank
External Organizations;

/persons/resource/fcotton

Cotton,  Fabrice
2.6 Seismic Hazard and Risk Dynamics, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Eibl,  Eva P. S.
External Organizations;

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5008179.pdf
(Postprint), 9MB

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Citation

Zali, Z., Ohrnberger, M., Scherbaum, F., Cotton, F., Eibl, E. P. S. (2021): Volcanic Tremor Extraction and Earthquake Detection Using Music Information Retrieval Algorithms. - Seismological Research Letters, 92, 6, 3668-3681.
https://doi.org/10.1785/0220210016


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5008179
Abstract
Volcanic tremor signals are usually observed before or during volcanic eruptions andmust be monitored to evaluate the volcanic activity. A challenge in studying seismic signals of volcanic origin is the coexistence of transient signal swarms and long-lasting volcanic tremor signals. Separating transient events fromvolcanic tremors can, therefore, contribute to improving upon our understanding of the underlying physical processes. Exploiting the idea of harmonic–percussive separation in musical signal processing, we develop a method to extract the harmonic volcanic tremor signals and to detect transient events from seismic recordings. Based on the similarity properties of spectrogram frames in the time–frequency domain, we decompose the signal into two separate spectrograms representing repeating (harmonic) and nonrepeating (transient) patterns, which correspond to volcanic tremor signals and earthquake signals, respectively. We reconstruct the harmonic tremor signal in the time domain from the complex spectrogram of the repeating pattern by only considering the phase components for the frequency range in which the tremor amplitude spectrum is significantly contributing to the energy of the signal. The reconstructed signal is, therefore, clean tremor signal without transient events. Furthermore, we derive a characteristic function suitable for the detection of transient events (e.g., earthquakes) by integrating amplitudes of the nonrepeating spectrogram over frequency at each time frame. Considering transient events like earthquakes, 78% of the events are detected for signal-to-noise ratio = 0.1 in our semisynthetic tests. In addition, we compared the number of detected earthquakes using our method for one month of continuous data recorded during the Holuhraun 2014–2015 eruption in Iceland with the bulletin presented in Ágústsdóttir et al. (2019). Our single station event detection algorithm identified 84% of the bulletin events. Moreover, we detected a total of 12,619 events, which is more than twice the number of the bulletin events.