Northern hemispheric winter warming pattern after tropical volcanic eruptions: Sensitivity to the ozone climatology

An important key for the understanding of the dynamic response to large tropical volcanic eruptions is the warming of the tropical lower stratosphere and the concomitant intensification of the polar vortices. Although this mechanism is reproduced by most general circulation models today, most models...

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Veröffentlicht in:Journal of geophysical research. Atmospheres 2014-02, Vol.119 (3), p.1340-1355
Hauptverfasser: Muthers, S., Anet, J. G., Raible, C. C., Brönnimann, S., Rozanov, E., Arfeuille, F., Peter, T., Shapiro, A. I., Beer, J., Steinhilber, F., Brugnara, Y., Schmutz, W.
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Sprache:eng
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