Stratospheric Aerosols from Major Volcanic Eruptions: A Composition-Climate Model Study of the Aerosol Cloud Dispersal and e-folding Time

Large explosive volcanic eruptions are capable of injecting considerable amounts of particles and sulfur gases above the tropopause, causing large increases in stratospheric aerosols. Five major volcanic eruptions after 1960 (i.e., Agung, St. Helens, El Chichón, Nevado del Ruiz and Pinatubo) have be...

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Auteurs principaux:	Giovanni Pitari, Glauco Di Genova, Eva Mancini, Daniele Visioni, Ilaria Gandolfi, Irene Cionni
Format:	Artigo
Langue:	Inglês
Publié:	MDPI AG 2016-05-01
Collection:	Atmosphere
Sujets:	composition-climate model explosive volcanic eruptions sulfate aerosols aerosol radiative efficiency stratospheric dynamics quasi-biennial oscillation
Accès en ligne:	http://www.mdpi.com/2073-4433/7/6/75
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