dor_id: 4132702

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/1122/1050

100.1.#.a: Clemesha, B.R.; Simonich, D.M

524.#.#.a: Clemesha, B.R., et al. (1994). Lidar observations of the El Chichón aerosol at a southern latitude station. Geofísica Internacional; Vol. 23 Núm. 2: Abril 1, 1984; 289-297. Recuperado de https://repositorio.unam.mx/contenidos/4132702

245.1.0.a: Lidar observations of the El Chichón aerosol at a southern latitude station

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1994

264.#.1.c: 1984-04-01

653.#.#.a: Aerosol estratosférico; Lidar; Erupciones volcánicas; Mediciones; Volcán El Chichón; Stratospheric aerosol; Lidar; Volcanic eruptions; Measurements; El Chichón Volcano

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/1122

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1122

041.#.7.h: spa

520.3.#.a: Lidar observations at Sao José dos Campos (23ºS, 46°W) show that the El Chichón dust cloud had reached this latitude by mid-July, 1982. The first measurement made after the eruption showed two layers with scattering ratios of 1.8 and 2. 7 at 18 and 24 km respectively, as compared with pre-injection values of about 1.2. These values refer to a wavelength of 5 890 Jl, and are for a profile obtained on July 9th. Measurements made in subsequent months showed large fluctuations, particularly in the upper !ayer, where the scattering ratio varied between 1.2 and 5. The lower !ayer varied much less than the upper, with the result that the integrated backscatter, a measure of the total stratospheric aerosol burden; remained roughly constant until late August, when it increased from about 3 x 10"4 SR-1 to about 1 x 10-3 SR-1 . Subsequent to this date the integrated aerosol oscillated around a value of about 8 x 10-4 SR-1 until midMarch 1983, since when it has decreased to about 5 x 10-4 SR-1 • The height of the upper !ayer decreased fairly uniformly with time until late November, when it reached 20 km, by which time it had merged with the lower layer. In 1983 the !ayer has again shown a bifurcated structure with a lower peak close to 18 km andan upper one 2 to 4 km higher.doi: https://doi.org/10.22201/igeof.00167169p.1984.23.2.843

773.1.#.t: Geofísica Internacional; Vol. 23 Núm. 2: Abril 1, 1984; 289-297

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: 289-297

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

doi: https://doi.org/10.22201/igeof.00167169p.1984.23.2.843

handle: 00b2907b54a6490b

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

856.#.0.q: application/pdf

file_creation_date: 2008-06-26 16:29:52.0

file_modification_date: 2022-05-29 04:25:34.0

file_creator: B.R. Clemesha

file_name: f67ef8195bf52ae306d33bf070401401174b8eba786260fa16937e73725c951c.pdf

file_pages_number: 9

file_format_version: application/pdf; version=1.6

file_size: 370176

245.1.0.b: Lidar observations of the El Chichón aerosol at a southern latitude station

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

Lidar observations of the El Chichón aerosol at a southern latitude station

Clemesha, B.R.; Simonich, D.M

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

Clemesha, B.R., et al. (1994). Lidar observations of the El Chichón aerosol at a southern latitude station. Geofísica Internacional; Vol. 23 Núm. 2: Abril 1, 1984; 289-297. Recuperado de https://repositorio.unam.mx/contenidos/4132702

Descripción del recurso

Autor(es)
Clemesha, B.R.; Simonich, D.M
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Lidar observations of the El Chichón aerosol at a southern latitude station
Fecha
1984-04-01
Resumen
Lidar observations at Sao José dos Campos (23ºS, 46°W) show that the El Chichón dust cloud had reached this latitude by mid-July, 1982. The first measurement made after the eruption showed two layers with scattering ratios of 1.8 and 2. 7 at 18 and 24 km respectively, as compared with pre-injection values of about 1.2. These values refer to a wavelength of 5 890 Jl, and are for a profile obtained on July 9th. Measurements made in subsequent months showed large fluctuations, particularly in the upper !ayer, where the scattering ratio varied between 1.2 and 5. The lower !ayer varied much less than the upper, with the result that the integrated backscatter, a measure of the total stratospheric aerosol burden; remained roughly constant until late August, when it increased from about 3 x 10"4 SR-1 to about 1 x 10-3 SR-1 . Subsequent to this date the integrated aerosol oscillated around a value of about 8 x 10-4 SR-1 until midMarch 1983, since when it has decreased to about 5 x 10-4 SR-1 • The height of the upper !ayer decreased fairly uniformly with time until late November, when it reached 20 km, by which time it had merged with the lower layer. In 1983 the !ayer has again shown a bifurcated structure with a lower peak close to 18 km andan upper one 2 to 4 km higher.doi: https://doi.org/10.22201/igeof.00167169p.1984.23.2.843
Tema
Aerosol estratosférico; Lidar; Erupciones volcánicas; Mediciones; Volcán El Chichón; Stratospheric aerosol; Lidar; Volcanic eruptions; Measurements; El Chichón Volcano
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces