Artículo

Detection of ionospheric response to earthquakes in Mexico: case study of September 8, 2021 and September 19, 2022

Melgarejo, Angela; Sergeeva, Maria A.; Kazachkina, Ekaterina; Vesnin, Artem M.; Aguilar-Rodriguez, Ernesto

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional y cosechado de y cosechado de Revistas UNAM

Licencia de uso

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. Ver términos de la licencia

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Melgarejo, Angela, et al. (2025). Detection of ionospheric response to earthquakes in Mexico: case study of September 8, 2021 and September 19, 2022. Geofísica Internacional; Vol. 64 Núm. 1: Enero 1, 2025; 1367-1378. Recuperado de https://repositorio.unam.mx/contenidos/4161287

Descripción del recurso

Autor(es)
Melgarejo, Angela; Sergeeva, Maria A.; Kazachkina, Ekaterina; Vesnin, Artem M.; Aguilar-Rodriguez, Ernesto
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Detection of ionospheric response to earthquakes in Mexico: case study of September 8, 2021 and September 19, 2022
Fecha
2025-01-01
Resumen
We explore the possibility of the ionospheric disturbance detection after two earthquakes (EQ) (Mw > 7) occurred on September 8, 2021, and September 19, 2022, in Mexico. The epicenter location, depth, focal mechanism, season and Space Weather background conditions were similar for the two EQs. The local time and the magnitude were different. Wave responses in the filtered slant TEC time series were revealed after both EQs at isolated satellite-receiver ray paths. The irregular variations exceeded the background fluctuation level and were not repeated on other days. Their form and temporal scales allowed us to associate them with the acoustic-gravity waves generated by the vertical displacement during the powerful EQs. The nighttime EQ on September 8, 2021, caused the medium-scale disturbances characterized with the N- and И-form fluctuations in TEC, a period of ~30 min and amplitudes of (0.1-0.2) TECU. The response to the daytime EQ on September 19, 2022, was of two types: smallscale disturbances N-, V-, И- and M-form with a 15 min period and amplitudes of (0.1-1.1) TECU; and medium-scale disturbances of N- and И-form with a period of ~30 min and amplitudes of (0.1-0.2) TECU. The presented conclusions for the Mexican region are preliminary as more statistics are needed.
Tema
perturbaciones ionosféricas co-sísmicas; TEC oblicuo; México; terremotos; co-seismic ionospheric disturbance; earthquakes; slant TEC; Mexico
Idioma
spa
ISSN
ISSN electrónico: 2954-436X; ISSN impreso: 0016-7169

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