dor_id: 4133250
506.#.#.a: Público
590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares
510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase
561.#.#.u: https://www.geofisica.unam.mx/
650.#.4.x: Físico Matemáticas y Ciencias de la Tierra
336.#.#.b: article
336.#.#.3: Artículo de Investigación
336.#.#.a: Artículo
351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI
351.#.#.b: Geofísica Internacional
351.#.#.a: Artículos
harvesting_group: RevistasUNAM
270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx
590.#.#.c: Open Journal Systems (OJS)
270.#.#.d: MX
270.1.#.d: México
590.#.#.b: Concentrador
883.#.#.u: https://revistas.unam.mx/catalogo/
883.#.#.a: Revistas UNAM
590.#.#.a: Coordinación de Difusión Cultural
883.#.#.1: https://www.publicaciones.unam.mx/
883.#.#.q: Dirección General de Publicaciones y Fomento Editorial
850.#.#.a: Universidad Nacional Autónoma de México
856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/48/44
100.1.#.a: Mendoza-rosas, Ana Teresa; De La Cruz Reyna, Servando
524.#.#.a: Mendoza-rosas, Ana Teresa, et al. (2019). Hazard assessment of the ongoing lava dome eruption at Popocatépetl volcano from the statistical analysis of significant explosive events in the period of 1997 to. Geofísica Internacional; Vol. 58 Núm. 1: Enero 1, 2019; 33-48. Recuperado de https://repositorio.unam.mx/contenidos/4133250
245.1.0.a: Hazard assessment of the ongoing lava dome eruption at Popocatépetl volcano from the statistical analysis of significant explosive events in the period of 1997 to
502.#.#.c: Universidad Nacional Autónoma de México
561.1.#.a: Instituto de Geofísica, UNAM
264.#.0.c: 2019
264.#.1.c: 2019-01-01
653.#.#.a: volcán Popocatépetl; erupción de domos de lava; explosiones vulcanianas; columnas eruptivas; emisión de cenizas; exhalaciones; análisis estadístico; Popocatépetl volcano; lava dome eruption; vulcanian explosions; eruptive columns; ash emission; exhalations; statistical analysis
506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx
884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/48
001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/48
041.#.7.h: spa
520.3.#.a: After 70 years of quiescence Popocatépetl volcano began a new episode of activity in 1994, which is still ongoing. The predominant activity has been a succession of dome emplacements followed by sequences of dome-destruction explosions producing prominent volcanic ash columns. Moreover, relatively large eruptive columns have also been produced during the dome growth stages. To assess the hazard of this activity we use the height of the columns as an indicator of the rate of energy release of the events and of their dispersive power and destructive potential. We hence built a database of the events producing columns exceeding heights of 4 km above the volcano summit for the period 1997 to 2016. Considering the occurrences of such columns as a random variable representing the hazard of such explosive activity, we studied the statistical features of the database, and found that the occurrence rate of significant explosions is a point process developing in at least two stages, with the significant changepoint in 2003. The first stage from 1997 to 2003 is non stationary, while the second one, from 2003 to 2016, shows a stationary behavior. While the former is well described by a Mixture of Exponentials distribution (MOED), the latter fits well an Exponential distribution. The probabilities of significant eruptive columns occurring in given time intervals result to be strongly dependent on the stationarity of the process. The assessment of hazard thus requires a continuous testing of the time dependence of the ongoing process, since there is no clear physical evidence of the factors controlling this behavior. doi: https://doi.org/10.22201/igeof.00167169p.2019.58.1.2065
773.1.#.t: Geofísica Internacional; Vol. 58 Núm. 1: Enero 1, 2019; 33-48
773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI
022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169
310.#.#.a: Trimestral
300.#.#.a: Páginas: 33-48
264.#.1.b: Instituto de Geofísica, UNAM
doi: https://doi.org/10.22201/igeof.00167169p.2019.58.1.2065
handle: 46e0de22b9875bab
harvesting_date: 2023-06-20 16:00:00.0
856.#.0.q: application/pdf
file_creation_date: 2019-03-01 18:18:23.0
file_modification_date: 2022-04-08 13:57:06.0
file_creator: Mendoza-Rosas A.T.
file_name: 95848396621f74ad31e2ac5540b4709ed3c642c35657621e84fb2fa91046e1d7.pdf
file_pages_number: 16
file_format_version: application/pdf; version=1.4
file_size: 6915507
245.1.0.b: Hazard assessment of the ongoing lava dome eruption at Popocatépetl volcano from the statistical analysis of significant explosive events in the period of 1997 to 2016
last_modified: 2023-06-20 16:00:00
license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es
license_type: by-nc-sa
No entro en nada
No entro en nada 2