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...
Published in: | Nature Communications |
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Main Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Nature Portfolio
2019
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Subjects: | |
Online Access: | https://doi.org/10.1038/s41467-019-08357-0 https://doaj.org/article/3f26a1e9d1264dd0a41899540dc15ac6 |
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. |
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