dor_id: 42032

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510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT), Sistema Regional de Información en Línea para Revistas Científicas de América Latina, el Caribe, España y Portugal (Latindex), Scientific Electronic Library Online (SciELO), SCOPUS, Web Of Science (WoS)

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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1158/1136

100.1.#.a: Galindo, Ignacio; Otaola, J. A.; Zenteno, G.

524.#.#.a: Galindo, Ignacio, et al. (1984). Atmospheric impact of the volcanic eruptions of el chichon over Mexico. Geofísica Internacional; Vol. 23 No. 3, 1984. Recuperado de https://repositorio.unam.mx/contenidos/42032

245.1.0.a: Atmospheric impact of the volcanic eruptions of el chichon over Mexico

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1984

264.#.1.c: 2013-04-12

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-ND 4.0 Internacional, https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode.es, fecha de asignación de la licencia 2013-04-12, para un uso diferente consultar al responsable jurídico del repositorio por medio de revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1158

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041.#.7.h: spa

520.3.#.a: In the present study we report the tropospheric effects observed on the Mexican territory of El Chichón volcano eruptions. We have used in the study, the air surface temperature records of five observatories as well as solar radiation and atmospheric turbidity measurements made in Mexico City. The results show that from May-June 1982 to March-April 1983, a temperature cooling trend was observed in all the Observatories, followed by an abrupt warming in the summer of 1983 concomitant to an important extinction of direct solar radiation and the corresponding elevation of atmospheric turbidity. The observed regional cooling is in agreement with the results of radiative transfer models on atmospheric effects of volcanic eruptions. The joint analysis of our results together with those reported from NASA aircraft observations and those of stratospheric balloons performed at the same time period, points out to the conclusion that this regional tropospheric warming associated to an important solar radiation extinction may be due to the massive descent into the troposphere of the stratospheric volcanic aerosols.

773.1.#.t: Geofísica Internacional; Vol. 23 No. 3 (1984)

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

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Artículo

Atmospheric impact of the volcanic eruptions of el chichon over Mexico

Galindo, Ignacio; Otaola, J. A.; Zenteno, 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

Galindo, Ignacio, et al. (1984). Atmospheric impact of the volcanic eruptions of el chichon over Mexico. Geofísica Internacional; Vol. 23 No. 3, 1984. Recuperado de https://repositorio.unam.mx/contenidos/42032

Descripción del recurso

Autor(es)
Galindo, Ignacio; Otaola, J. A.; Zenteno, G.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Atmospheric impact of the volcanic eruptions of el chichon over Mexico
Fecha
2013-04-12
Resumen
In the present study we report the tropospheric effects observed on the Mexican territory of El Chichón volcano eruptions. We have used in the study, the air surface temperature records of five observatories as well as solar radiation and atmospheric turbidity measurements made in Mexico City. The results show that from May-June 1982 to March-April 1983, a temperature cooling trend was observed in all the Observatories, followed by an abrupt warming in the summer of 1983 concomitant to an important extinction of direct solar radiation and the corresponding elevation of atmospheric turbidity. The observed regional cooling is in agreement with the results of radiative transfer models on atmospheric effects of volcanic eruptions. The joint analysis of our results together with those reported from NASA aircraft observations and those of stratospheric balloons performed at the same time period, points out to the conclusion that this regional tropospheric warming associated to an important solar radiation extinction may be due to the massive descent into the troposphere of the stratospheric volcanic aerosols.
Idioma
spa
ISSN
0016-7169

Enlaces