dor_id: 4133425

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/367/1468

100.1.#.a: De Artigas, Marta Zossi; Ortiz De Adler, Nieves; Elias, Ana G.

524.#.#.a: De Artigas, Marta Zossi, et al. (2004). Ionospheric response to the equatorial stratospheric wind. Geofísica Internacional; Vol. 43 Núm. 2: Abril 1, 2004; 199-203. Recuperado de https://repositorio.unam.mx/contenidos/4133425

245.1.0.a: Ionospheric response to the equatorial stratospheric wind

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2004

264.#.1.c: 2004-04-01

653.#.#.a: Efecto dinamo; Frecuencia crítica de la capa F2; Monthly mean zonal wind; Quasi-biennial oscillation; Dynamo effect; F2 layer critical frequency; Monthly mean zonal wind; Quasi-biennial oscillation

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/367

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/367

041.#.7.h: spa

520.3.#.a: Chen (1992) reports an association between the variance of the F2 layer critical frequency, foF2var, and the quasi-biennial oscillation, QBO, of the monthly mean zonal wind in the equatorial stratosphere (MMZW) at 40 mb, with data of March and September at Okinawa (26°N, 128°E). We search for such an association in other locations. Monthly-hourly foF2 data (between 12 and 19 LT) for the period 1957-1989 from Tucumán (27°S; 65°W), at the southern equatorial anomaly crest at the magnetic equator (Huancayo,12°S; 75°W), and in high latitude (Slough, 51°N; 0.6°W) were analyzed. The correlation coefficient between foF2var and MMZW is 0.05, 0.16 and 0.20 for Tucumán, Huancayo and Slough respectively, suggesting that there is no association. However, the correlation coefficient for Okinawa (r=0.65), and for Tucumán in the period 1958-1968 (r=0.67 , is high. We do not rule out the possibility that the QBO of MMZW modulates the ionosphere at the crests of the equatorial anomaly. We look for an explanation of the loss of correlation for Tucumán after 1968. Spectral analysis, for all three stations, shows a significant high-frequency oscillation in foF2var (2.5-3.3 years) which is very close but not coincident with the QBO present in MMZW.doi: sin doi

773.1.#.t: Geofísica Internacional; Vol. 43 Núm. 2: Abril 1, 2004; 199-203

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: 199-203

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.2004.43.2.367

handle: 00d508e3d2346b0f

harvesting_date: 2023-06-20 16:00:00.0

856.#.0.q: application/pdf

file_creation_date: 2022-08-12 15:51:41.0

file_modification_date: 2022-08-12 15:55:51.0

file_creator: Marta Zossi de Artigas

file_name: a85638dc31d96e81e67a8040a75bb37fb0db930cbf0c6d714903af7de5669a57.pdf

file_pages_number: 5

file_format_version: application/pdf; version=1.7

file_size: 2200497

245.1.0.b: Ionospheric response to the equatorial stratospheric wind

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

Artículo

Ionospheric response to the equatorial stratospheric wind

De Artigas, Marta Zossi; Ortiz De Adler, Nieves; Elias, Ana G.

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

Licencia de uso

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

De Artigas, Marta Zossi, et al. (2004). Ionospheric response to the equatorial stratospheric wind. Geofísica Internacional; Vol. 43 Núm. 2: Abril 1, 2004; 199-203. Recuperado de https://repositorio.unam.mx/contenidos/4133425

Descripción del recurso

Autor(es)
De Artigas, Marta Zossi; Ortiz De Adler, Nieves; Elias, Ana G.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Ionospheric response to the equatorial stratospheric wind
Fecha
2004-04-01
Resumen
Chen (1992) reports an association between the variance of the F2 layer critical frequency, foF2var, and the quasi-biennial oscillation, QBO, of the monthly mean zonal wind in the equatorial stratosphere (MMZW) at 40 mb, with data of March and September at Okinawa (26°N, 128°E). We search for such an association in other locations. Monthly-hourly foF2 data (between 12 and 19 LT) for the period 1957-1989 from Tucumán (27°S; 65°W), at the southern equatorial anomaly crest at the magnetic equator (Huancayo,12°S; 75°W), and in high latitude (Slough, 51°N; 0.6°W) were analyzed. The correlation coefficient between foF2var and MMZW is 0.05, 0.16 and 0.20 for Tucumán, Huancayo and Slough respectively, suggesting that there is no association. However, the correlation coefficient for Okinawa (r=0.65), and for Tucumán in the period 1958-1968 (r=0.67 , is high. We do not rule out the possibility that the QBO of MMZW modulates the ionosphere at the crests of the equatorial anomaly. We look for an explanation of the loss of correlation for Tucumán after 1968. Spectral analysis, for all three stations, shows a significant high-frequency oscillation in foF2var (2.5-3.3 years) which is very close but not coincident with the QBO present in MMZW.doi: sin doi
Tema
Efecto dinamo; Frecuencia crítica de la capa F2; Monthly mean zonal wind; Quasi-biennial oscillation; Dynamo effect; F2 layer critical frequency; Monthly mean zonal wind; Quasi-biennial oscillation
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces