Articles | Volume 17, issue 2
Clim. Past, 17, 633–652, 2021

Special issue: Interdisciplinary studies of volcanic impacts on climate and...

Clim. Past, 17, 633–652, 2021
Research article
11 Mar 2021
Research article | 11 Mar 2021

Simulation of ash clouds after a Laacher See-type eruption

Ulrike Niemeier et al.

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Cited articles

Abbott, P. M. and Davies, S. M.: Volcanism and the Greenland ice-cores: the tephra record, Earth-Sci. Rev., 115, 173–191,, 2012. a
Andrews, D. G., Holton, J. R., and Leovy, C. B.: Middle Atmosphere Dynamics, Academic Press, San Diego, CA, 1987. a
Aquila, V., Oman, L. D., Stolarski, R. S., Colarco, P. R., and Newman, P. A.: Dispersion of the volcanic sulfate cloud from a Mount Pinatubo-like eruption, J. Geophys. Res-Atmos., 117, D06216,, 2012. a
Aspinall, W. and Woo, G.: Counterfactual Analysis of Runaway Volcanic Explosions, Front. Earth Sci., 7, 222,, 2019. a
Baales, M., Jöris, O., Street, M., Bittmann, F., Weninger, B., and Wiethold, J.: Impact of the Late Glacial Eruption of the Laacher See Volcano, Central Rhineland, Germany, Quaternary Res., 58, 273–288,, 2002. a, b, c
Short summary
The 13 kyr BP Laacher See eruption impacted local environments, human communities and climate. We have simulated the evolution of its fine ash and sulfur cloud such that it reflects the empirically known ash distribution. In our models, the heating of the ash causes a mesocyclone which changes the dispersion of the cloud itself, resulting in enhanced transport to low latitudes. This may partially explain why no Laacher See ash has yet been found in Greenlandic ice cores.