2600-years of stratospheric volcanism through sulfate isotopes

The estimation of volcanic contribution to climate variability requires identification of global-scale eruptions. Here the authors present a new 2600-year chronology of stratospheric volcanic events that relies on isotopic signature of ice core sulfate, that improves ice core volcanic reconstruction...

Full description

Bibliographic Details
Published in:Nature Communications
Main Authors: E. Gautier, J. Savarino, J. Hoek, J. Erbland, N. Caillon, S. Hattori, N. Yoshida, E. Albalat, F. Albarede, J. Farquhar
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2019
Subjects:
Science
Q
ice core
Online Access:https://doi.org/10.1038/s41467-019-08357-0
https://doaj.org/article/3f26a1e9d1264dd0a41899540dc15ac6
Description
Summary:The estimation of volcanic contribution to climate variability requires identification of global-scale eruptions. Here the authors present a new 2600-year chronology of stratospheric volcanic events that relies on isotopic signature of ice core sulfate, that improves ice core volcanic reconstruction.

Similar Items