Articles | Volume 12, issue 4
https://doi.org/10.5194/cp-12-961-2016
https://doi.org/10.5194/cp-12-961-2016
Research article
 | 
15 Apr 2016
Research article |  | 15 Apr 2016

The influence of volcanic eruptions on the climate of tropical South America during the last millennium in an isotope-enabled general circulation model

Christopher M. Colose, Allegra N. LeGrande, and Mathias Vuille

Viewed

Total article views: 4,816 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,042 1,564 210 4,816 555 162 200
  • HTML: 3,042
  • PDF: 1,564
  • XML: 210
  • Total: 4,816
  • Supplement: 555
  • BibTeX: 162
  • EndNote: 200
Views and downloads (calculated since 23 Jul 2015)
Cumulative views and downloads (calculated since 23 Jul 2015)

Cited

Saved (preprint)

Discussed (final revised paper)

Latest update: 13 Dec 2024
Download
Short summary
Volcanic forcing is the most important source of forced variability during the preindustrial component of the last millennium (~ 850-1850 CE) and is important during the last century.

Here, we focus on the climate impact over South America in a model-based study. Emphasis is given to temperature, precipitation, and oxygen isotope variability (allowing for potential contact made with paleoclimate-based observations)