Articles | Volume 21, issue 10
https://doi.org/10.5194/cp-21-1755-2025
https://doi.org/10.5194/cp-21-1755-2025
Research article
 | 
20 Oct 2025
Research article |  | 20 Oct 2025

Using reduced-complexity volcanic aerosol and climate models to produce large ensemble simulations of Holocene temperature

Magali Verkerk, Thomas J. Aubry, Chris Smith, Peter O. Hopcroft, Michael Sigl, Jessica E. Tierney, Kevin Anchukaitis, Matthew Osman, Anja Schmidt, and Matthew Toohey

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Short summary
Large volcanic eruptions can trigger global cooling, affecting human societies. Using ice-core records and simple climate model to simulate volcanic effect over the last 8500 years, we show that volcanic eruptions cool the climate by 0.12 °C on average. By comparing model results with temperature recorded by tree rings over the last 1000 years, we demonstrate that our models can predict the large-scale cooling caused by volcanic eruptions and can be used in cases of large eruptions in the future.
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