dor_id: 4132619

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

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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

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883.#.#.a: Revistas UNAM

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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/1154/1074

100.1.#.a: Vupputuri, R.K.R.; Blanchet, J.P.

524.#.#.a: Vupputuri, R.K.R., et al. (1984). The possible effects of El Chichon eruption on atmospheric thermal and chemical structure and surface climate. Geofísica Internacional; Vol. 23 Núm. 3: Julio 1, 1984; 433-447. Recuperado de https://repositorio.unam.mx/contenidos/4132619

245.1.0.a: The possible effects of El Chichon eruption on atmospheric thermal and chemical structure and surface climate

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1984

264.#.1.c: 1984-07-01

653.#.#.a: Térmica atmosférica; Estructura química; Clima superficial; Efectos; Erupciones volcánicas; Volcán El Chichón; Atmospheric thermal; Chemical structure; Surface climate; Efffects; Volcanic eruptions; El Chichon 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/1154

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1154

041.#.7.h: spa

520.3.#.a: It is suggested that the injection of sulfur oxides and ash into the stratosphere from 1982 El Chichón eruption, would alter the radiative-photochemical balance of the earth"s atmosphere which in turn leads to the changes in the vertical temperature and chemical structure -0f the at mosphere and surface climate. In this study one dimensional radiative-convective-photochemical model is used to compute the thermal and chemical response of the atmosphere and the surface climate to enhanced stratospheric aerosol concentrations resulting from the El Chichón eruption. The recent observational data on aerosol optical thickness and optical properties obtained from the global monitoring of the El Chichón cloud has been used as input to model integration. The model allows variable aerosol concentrations and optical properties in time during the life cycle of the volcanic cloud.The preliminary results show that during the first year after the eruption, the global average surface temperature decreases by about 0.9°C while causing significant warming in the lower stratosphere (up to 5°C). The atmosphere and the surface will reach their background teMperature values within roughly 3 to 4 years after the eruption. Also discussed are the implications of El Chichón eruption to stratospheric ozone photochemical cycle.doi: https://doi.org/10.22201/igeof.00167169p.1984.23.3.1162

773.1.#.t: Geofísica Internacional; Vol. 23 Núm. 3: Julio 1, 1984; 433-447

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: 433-447

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

doi: https://doi.org/10.22201/igeof.00167169p.1984.23.3.1162

handle: 00f52f03aa249846

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

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file_creator: R.K.R. Vupputuri

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245.1.0.b: The possible effects of El Chichon eruption on atmospheric thermal and chemical structure and surface climate

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Artículo

The possible effects of El Chichon eruption on atmospheric thermal and chemical structure and surface climate

Vupputuri, R.K.R.; Blanchet, J.P.

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

Vupputuri, R.K.R., et al. (1984). The possible effects of El Chichon eruption on atmospheric thermal and chemical structure and surface climate. Geofísica Internacional; Vol. 23 Núm. 3: Julio 1, 1984; 433-447. Recuperado de https://repositorio.unam.mx/contenidos/4132619

Descripción del recurso

Autor(es)
Vupputuri, R.K.R.; Blanchet, J.P.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
The possible effects of El Chichon eruption on atmospheric thermal and chemical structure and surface climate
Fecha
1984-07-01
Resumen
It is suggested that the injection of sulfur oxides and ash into the stratosphere from 1982 El Chichón eruption, would alter the radiative-photochemical balance of the earth"s atmosphere which in turn leads to the changes in the vertical temperature and chemical structure -0f the at mosphere and surface climate. In this study one dimensional radiative-convective-photochemical model is used to compute the thermal and chemical response of the atmosphere and the surface climate to enhanced stratospheric aerosol concentrations resulting from the El Chichón eruption. The recent observational data on aerosol optical thickness and optical properties obtained from the global monitoring of the El Chichón cloud has been used as input to model integration. The model allows variable aerosol concentrations and optical properties in time during the life cycle of the volcanic cloud.The preliminary results show that during the first year after the eruption, the global average surface temperature decreases by about 0.9°C while causing significant warming in the lower stratosphere (up to 5°C). The atmosphere and the surface will reach their background teMperature values within roughly 3 to 4 years after the eruption. Also discussed are the implications of El Chichón eruption to stratospheric ozone photochemical cycle.doi: https://doi.org/10.22201/igeof.00167169p.1984.23.3.1162
Tema
Térmica atmosférica; Estructura química; Clima superficial; Efectos; Erupciones volcánicas; Volcán El Chichón; Atmospheric thermal; Chemical structure; Surface climate; Efffects; Volcanic eruptions; El Chichon Volcano
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

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