Permutation entropy variation for 2007 effusive dome-forming eruption period of Kelud Volcano, Indonesia

The complexity of a system recorded in time series data can be measured statistically using permutation entropy (PE). The state of a system (e.g. regular, chaotic, random, etc.) that underlies the appearance of variations in time series can be determined with PE. Since volcanoes are considered as th...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	Nugraheni Lusia Rita, Harijoko Agung, Suryanto Wiwit, Triastuty Hetty
Formato:	article
Lenguaje:	EN FR
Publicado:	EDP Sciences 2021
Materias:	Environmental sciences GE1-350
Acceso en línea:	https://doaj.org/article/f3885f7e2ae94344a0f2cf66438c9d8f
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:f3885f7e2ae94344a0f2cf66438c9d8f
record_format	dspace
spelling	oai:doaj.org-article:f3885f7e2ae94344a0f2cf66438c9d8f2021-12-02T17:11:56ZPermutation entropy variation for 2007 effusive dome-forming eruption period of Kelud Volcano, Indonesia2267-124210.1051/e3sconf/202132501010https://doaj.org/article/f3885f7e2ae94344a0f2cf66438c9d8f2021-01-01T00:00:00Zhttps://www.e3s-conferences.org/articles/e3sconf/pdf/2021/101/e3sconf_icst2021_01010.pdfhttps://doaj.org/toc/2267-1242The complexity of a system recorded in time series data can be measured statistically using permutation entropy (PE). The state of a system (e.g. regular, chaotic, random, etc.) that underlies the appearance of variations in time series can be determined with PE. Since volcanoes are considered as the complex dynamical system controlled by interactions of many processes. Permutation entropy can be applied to study the system mechanism of volcano. We utilized PE to study system mechanism of Kelud volcano in 2007 dome-forming eruption period, from 3 (KWH; KLD; UMBK) seismic stations with different distances from the crater lake. Then, we want to compare the results. The result of study shows that the PE pattern for each station is different. The unique PE pattern that can be used as an eruption precursor is only shown at KWH and KLD stations. This pattern began to appear 2.7 days before the eruption on 3 November 2007. Data from UMBK station doesn’t show unique PE pattern. The factors such as sensor distance from magmatic activity center, size, and type of eruption probably influenced the final PE result. Using PE as the addition to volcano monitoring can maximize efforts in mitigation activities.Nugraheni Lusia RitaHarijoko AgungSuryanto WiwitTriastuty HettyEDP SciencesarticleEnvironmental sciencesGE1-350ENFRE3S Web of Conferences, Vol 325, p 01010 (2021)
institution	DOAJ
collection	DOAJ
language	EN FR
topic	Environmental sciences GE1-350
spellingShingle	Environmental sciences GE1-350 Nugraheni Lusia Rita Harijoko Agung Suryanto Wiwit Triastuty Hetty Permutation entropy variation for 2007 effusive dome-forming eruption period of Kelud Volcano, Indonesia
description	The complexity of a system recorded in time series data can be measured statistically using permutation entropy (PE). The state of a system (e.g. regular, chaotic, random, etc.) that underlies the appearance of variations in time series can be determined with PE. Since volcanoes are considered as the complex dynamical system controlled by interactions of many processes. Permutation entropy can be applied to study the system mechanism of volcano. We utilized PE to study system mechanism of Kelud volcano in 2007 dome-forming eruption period, from 3 (KWH; KLD; UMBK) seismic stations with different distances from the crater lake. Then, we want to compare the results. The result of study shows that the PE pattern for each station is different. The unique PE pattern that can be used as an eruption precursor is only shown at KWH and KLD stations. This pattern began to appear 2.7 days before the eruption on 3 November 2007. Data from UMBK station doesn’t show unique PE pattern. The factors such as sensor distance from magmatic activity center, size, and type of eruption probably influenced the final PE result. Using PE as the addition to volcano monitoring can maximize efforts in mitigation activities.
format	article
author	Nugraheni Lusia Rita Harijoko Agung Suryanto Wiwit Triastuty Hetty
author_facet	Nugraheni Lusia Rita Harijoko Agung Suryanto Wiwit Triastuty Hetty
author_sort	Nugraheni Lusia Rita
title	Permutation entropy variation for 2007 effusive dome-forming eruption period of Kelud Volcano, Indonesia
title_short	Permutation entropy variation for 2007 effusive dome-forming eruption period of Kelud Volcano, Indonesia
title_full	Permutation entropy variation for 2007 effusive dome-forming eruption period of Kelud Volcano, Indonesia
title_fullStr	Permutation entropy variation for 2007 effusive dome-forming eruption period of Kelud Volcano, Indonesia
title_full_unstemmed	Permutation entropy variation for 2007 effusive dome-forming eruption period of Kelud Volcano, Indonesia
title_sort	permutation entropy variation for 2007 effusive dome-forming eruption period of kelud volcano, indonesia
publisher	EDP Sciences
publishDate	2021
url	https://doaj.org/article/f3885f7e2ae94344a0f2cf66438c9d8f
work_keys_str_mv	AT nugrahenilusiarita permutationentropyvariationfor2007effusivedomeformingeruptionperiodofkeludvolcanoindonesia AT harijokoagung permutationentropyvariationfor2007effusivedomeformingeruptionperiodofkeludvolcanoindonesia AT suryantowiwit permutationentropyvariationfor2007effusivedomeformingeruptionperiodofkeludvolcanoindonesia AT triastutyhetty permutationentropyvariationfor2007effusivedomeformingeruptionperiodofkeludvolcanoindonesia
_version_	1718381472453230592

Permutation entropy variation for 2007 effusive dome-forming eruption period of Kelud Volcano, Indonesia

Ejemplares similares