Articles | Volume 17, issue 1
https://doi.org/10.5194/acp-17-485-2017
https://doi.org/10.5194/acp-17-485-2017
Research article
 | 
11 Jan 2017
Research article |  | 11 Jan 2017

Revisiting the observed surface climate response to large volcanic eruptions

Fabian Wunderlich and Daniel M. Mitchell

Viewed

Total article views: 3,269 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,861 1,134 274 3,269 733 92 93
  • HTML: 1,861
  • PDF: 1,134
  • XML: 274
  • Total: 3,269
  • Supplement: 733
  • BibTeX: 92
  • EndNote: 93
Views and downloads (calculated since 22 Mar 2016)
Cumulative views and downloads (calculated since 22 Mar 2016)

Cited

Saved (preprint)

Discussed (final revised paper)

Latest update: 23 Nov 2024
Download
Short summary
Large volcanic eruptions can eject aerosols into the stratosphere and prevent UV radiation reaching the surface, resulting in surface cooling. A secondary, non-linear effect occurs at high latitudes. While the surface cooling is robust in observations, we show that the non-linear, high-latitude effect is less robust. Climate models have failures at reproducing both aspects, probably because of aliasing with other climate modes and overrepresentation of stratospheric aerosol.
Altmetrics
Final-revised paper
Preprint