Articles | Volume 15, issue 2
Clim. Past, 15, 685–700, 2019
https://doi.org/10.5194/cp-15-685-2019
Clim. Past, 15, 685–700, 2019
https://doi.org/10.5194/cp-15-685-2019
Research article
05 Apr 2019
Research article | 05 Apr 2019

Siberian tree-ring and stable isotope proxies as indicators of temperature and moisture changes after major stratospheric volcanic eruptions

Olga V. Churakova (Sidorova) et al.

Viewed

Total article views: 3,404 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,480 856 68 3,404 332 60 66
  • HTML: 2,480
  • PDF: 856
  • XML: 68
  • Total: 3,404
  • Supplement: 332
  • BibTeX: 60
  • EndNote: 66
Views and downloads (calculated since 27 Jun 2018)
Cumulative views and downloads (calculated since 27 Jun 2018)

Viewed (geographical distribution)

Total article views: 3,404 (including HTML, PDF, and XML) Thereof 3,123 with geography defined and 281 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 27 Nov 2022
Download
Short summary
We present a unique dataset of multiple tree-ring and stable isotope parameters, representing temperature-sensitive Siberian ecotones, to assess climatic impacts after six large stratospheric volcanic eruptions at 535, 540, 1257, 1640, 1815, and 1991 CE. Besides the well-documented effects of temperature derived from tree-ring width and latewood density, stable carbon and oxygen isotopes in tree-ring cellulose provide information about moisture and sunshine duration changes after the events.