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

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336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

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270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

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850.#.#.a: Universidad Nacional Autónoma de México

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100.1.#.a: Antuña, Juan Carlos; Pomares, Ismael; Estevan, René

524.#.#.a: Antuña, Juan Carlos, et al. (1996). Temperature trends at Camaguey, Cuba, after some volcanic eruptions. Atmósfera; Vol. 9 No. 4, 1996. Recuperado de https://repositorio.unam.mx/contenidos/4122234

245.1.0.a: Temperature trends at Camaguey, Cuba, after some volcanic eruptions

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

561.1.#.a: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM

264.#.0.c: 1996

264.#.1.c: 2009-10-05

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 4.0 Internacional, https://creativecommons.org/licenses/by-nc/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico editora@atmosfera.unam.mx

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041.#.7.h: eng

520.3.#.a: Temperature trends in the three years following the volcanic eruptions of Agung, El Chichón and Pinatubo are studied, employing monthly mean temperature data from four meteorological stations of the Meteorological Poligon of Camaguey (PMC). A descendent tendency was found for monthly mean temperature following those eruptions In general the trends in the three years following the eruptions are different, at a significative level of 99.5% from the trends of the entire data periods, revealing the cooling effects of those eruptions. Also in the Agung and El Chichón case the trends were significatively different at a 90% level, from the null trends. Different cooling effects between Pinatubo eruption and Agung and El Chichon eruptions are explained by the particularities of the movement of the stratospheric aerosols plume of the first, occasioned by the different epochs of the year in wich Pinatubo erupted respect to Agung and El Chichón. The evaluation of the temperature anomalies registered in the PMC in the year following the eruptions show a most intense cooling than in the Northern Hemisphere as a whole, reinforcing the hypothesis of the particular acentuate response of the PMC and probably for an island as Cuba to the shadowing of solar radiation by stratospheric aerosols, as result of its particular thermal insulation occasioned by the notable difference between the thermal capacities of the land and sea.

773.1.#.t: Atmósfera; Vol. 9 No. 4 (1996)

773.1.#.o: https://www.revistascca.unam.mx/atm/index.php/atm/index

046.#.#.j: 2021-10-20 00:00:00.000000

022.#.#.a: ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

310.#.#.a: Trimestral

264.#.1.b: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM

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

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245.1.0.b: Temperature trends at Camaguey, Cuba, after some volcanic eruptions

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Artículo

Temperature trends at Camaguey, Cuba, after some volcanic eruptions

Antuña, Juan Carlos; Pomares, Ismael; Estevan, René

Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM, publicado en Atmósfera, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Antuña, Juan Carlos, et al. (1996). Temperature trends at Camaguey, Cuba, after some volcanic eruptions. Atmósfera; Vol. 9 No. 4, 1996. Recuperado de https://repositorio.unam.mx/contenidos/4122234

Descripción del recurso

Autor(es)
Antuña, Juan Carlos; Pomares, Ismael; Estevan, René
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Temperature trends at Camaguey, Cuba, after some volcanic eruptions
Fecha
2009-10-05
Resumen
Temperature trends in the three years following the volcanic eruptions of Agung, El Chichón and Pinatubo are studied, employing monthly mean temperature data from four meteorological stations of the Meteorological Poligon of Camaguey (PMC). A descendent tendency was found for monthly mean temperature following those eruptions In general the trends in the three years following the eruptions are different, at a significative level of 99.5% from the trends of the entire data periods, revealing the cooling effects of those eruptions. Also in the Agung and El Chichón case the trends were significatively different at a 90% level, from the null trends. Different cooling effects between Pinatubo eruption and Agung and El Chichon eruptions are explained by the particularities of the movement of the stratospheric aerosols plume of the first, occasioned by the different epochs of the year in wich Pinatubo erupted respect to Agung and El Chichón. The evaluation of the temperature anomalies registered in the PMC in the year following the eruptions show a most intense cooling than in the Northern Hemisphere as a whole, reinforcing the hypothesis of the particular acentuate response of the PMC and probably for an island as Cuba to the shadowing of solar radiation by stratospheric aerosols, as result of its particular thermal insulation occasioned by the notable difference between the thermal capacities of the land and sea.
Idioma
eng
ISSN
ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

Enlaces