Subdiffusion of volcanic earthquakes

© 2017 Institute of Geophysics, Polish Academy of Sciences & Polish Academy of SciencesA comparative study is performed on volcanic seismicities at Icelandic volcano, Eyjafjallajökull, and Mt. Etna in Sicily from the viewpoint of complex systems science, and the discovery of remarkable similarit...

Full description

Bibliographic Details
Main Authors: Abe S., Suzuki N.
Format: Other/Unknown Material
Language:unknown
Published: 2017
Subjects:
Online Access:https://openrepository.ru/article?id=184501
id ftneicon:oai:rour.neicon.ru:rour/184501
record_format openpolar
spelling ftneicon:oai:rour.neicon.ru:rour/184501 2023-05-15T16:09:34+02:00 Subdiffusion of volcanic earthquakes Abe S. Suzuki N. 2017 https://openrepository.ru/article?id=184501 unknown Acta Geophysica 1 http://rour.neicon.ru:80/xmlui/bitstream/rour/184501/1/nora.pdf 1895-6572 https://openrepository.ru/article?id=184501 SCOPUS18956572-2017-SID85016112799 (Non-)Markovianity Exponential jump probability distributions Finite-dada-size effects Power-law waiting-time distributions Subdiffusion Volcanic seismicity Article in Press 2017 ftneicon 2020-07-21T12:02:04Z © 2017 Institute of Geophysics, Polish Academy of Sciences & Polish Academy of SciencesA comparative study is performed on volcanic seismicities at Icelandic volcano, Eyjafjallajökull, and Mt. Etna in Sicily from the viewpoint of complex systems science, and the discovery of remarkable similarities between them is reported. In these seismicities as point processes, the jump probability distributions of earthquakes (i.e., distributions of the distance between the hypocenters of two successive events) are found to obey the exponential law, whereas the waiting-time distributions (i.e., distributions of inter-occurrence time of two successive events) follow the power law. A careful analysis is made about the finite size effects on the waiting-time distributions, and the previously reported results for Mt. Etna (Abe and Suzuki 2015) are reinterpreted accordingly. It is shown that the growth of the seismic region in time is subdiffusive at both volcanoes. The aging phenomenon is commonly observed in the “event-time-averaged” mean-squared displacements of the hypocenters. A comment is also made on (non-)Markovianity of the processes. Other/Unknown Material Eyjafjallajökull NORA (National aggregator of open repositories of Russian universities)
institution Open Polar
collection NORA (National aggregator of open repositories of Russian universities)
op_collection_id ftneicon
language unknown
topic (Non-)Markovianity
Exponential jump probability distributions
Finite-dada-size effects
Power-law waiting-time distributions
Subdiffusion
Volcanic seismicity
spellingShingle (Non-)Markovianity
Exponential jump probability distributions
Finite-dada-size effects
Power-law waiting-time distributions
Subdiffusion
Volcanic seismicity
Abe S.
Suzuki N.
Subdiffusion of volcanic earthquakes
topic_facet (Non-)Markovianity
Exponential jump probability distributions
Finite-dada-size effects
Power-law waiting-time distributions
Subdiffusion
Volcanic seismicity
description © 2017 Institute of Geophysics, Polish Academy of Sciences & Polish Academy of SciencesA comparative study is performed on volcanic seismicities at Icelandic volcano, Eyjafjallajökull, and Mt. Etna in Sicily from the viewpoint of complex systems science, and the discovery of remarkable similarities between them is reported. In these seismicities as point processes, the jump probability distributions of earthquakes (i.e., distributions of the distance between the hypocenters of two successive events) are found to obey the exponential law, whereas the waiting-time distributions (i.e., distributions of inter-occurrence time of two successive events) follow the power law. A careful analysis is made about the finite size effects on the waiting-time distributions, and the previously reported results for Mt. Etna (Abe and Suzuki 2015) are reinterpreted accordingly. It is shown that the growth of the seismic region in time is subdiffusive at both volcanoes. The aging phenomenon is commonly observed in the “event-time-averaged” mean-squared displacements of the hypocenters. A comment is also made on (non-)Markovianity of the processes.
format Other/Unknown Material
author Abe S.
Suzuki N.
author_facet Abe S.
Suzuki N.
author_sort Abe S.
title Subdiffusion of volcanic earthquakes
title_short Subdiffusion of volcanic earthquakes
title_full Subdiffusion of volcanic earthquakes
title_fullStr Subdiffusion of volcanic earthquakes
title_full_unstemmed Subdiffusion of volcanic earthquakes
title_sort subdiffusion of volcanic earthquakes
publishDate 2017
url https://openrepository.ru/article?id=184501
genre Eyjafjallajökull
genre_facet Eyjafjallajökull
op_source SCOPUS18956572-2017-SID85016112799
op_relation Acta Geophysica
1
http://rour.neicon.ru:80/xmlui/bitstream/rour/184501/1/nora.pdf
1895-6572
https://openrepository.ru/article?id=184501
_version_ 1766405435064057856