Climate model simulations of the effects of the El Chichon eruption

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Publicado: jul 1, 1984
DOI: https://doi.org/10.22201/igeof.00167169p.1984.23.3.1160
Palabras clave:
Modelos climáticos, Simulaciones, Efectos, Erupciones volcánicas, Volcán El Chichón

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A. Robock
Department of Meteorology, University of Maryland, College Park, Maryland 20742, U.S.A.

Resumen

Se emplea un modelo climático de balance de energía para calcular el efecto de la erupción del 4 de abril de 1982 del volcán ~ Chichón sobre la temperatura del aire para los siguientes 10 años. El máximo enfriamiento de 1.0 - 1.4 C ocurre en el Polo Norte en la primavera y el otoño de 1984 y 1985. La respuesta promedio anual en el Hemisferio Norte es mayor en 1984 y 1985 con un enfriamiento de 0.4 - 0.5 C. Se presentan las respuestas de la tierra y del océano por separado corno funciones de latitud y época del año. Los patrones particulares que resultan son causados por las retroalimentaciones del albedo de la nieve y la inercia térmica del hielo. Estos resultados tienen implicaciones de importancia para la detección del cambio de clima inducido por el CO2.

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Robock, A. (1984). Climate model simulations of the effects of the El Chichon eruption. Geofísica Internacional, 23(3), 403–414. https://doi.org/10.22201/igeof.00167169p.1984.23.3.1160
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Vol. 23 Núm. 3 (1984): Julio 1, 1984
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Esta obra está bajo una licencia internacional Creative Commons Atribución-NoComercial-CompartirIgual 4.0.

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