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...
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2019-01-01
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Online Access: | https://doi.org/10.1038/s41467-019-08357-0 |
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doaj-3f26a1e9d1264dd0a41899540dc15ac62021-05-11T11:37:50ZengNature Publishing GroupNature Communications2041-17232019-01-011011710.1038/s41467-019-08357-02600-years of stratospheric volcanism through sulfate isotopesE. Gautier0J. Savarino1J. Hoek2J. Erbland3N. Caillon4S. Hattori5N. Yoshida6E. Albalat7F. Albarede8J. Farquhar9Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, Institut des Géosciences de l’Environnement (IGE)Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, Institut des Géosciences de l’Environnement (IGE)Department of Geology and Earth System Science Interdisciplinary Center (ESSIC), University of MarylandUniv. Grenoble Alpes, CNRS, IRD, Grenoble INP, Institut des Géosciences de l’Environnement (IGE)Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, Institut des Géosciences de l’Environnement (IGE)Department of Chemical Science and Engineering, School of Materials and Chemical Technology, Tokyo Institute of TechnologyDepartment of Chemical Science and Engineering, School of Materials and Chemical Technology, Tokyo Institute of TechnologyEcole Normale Supérieure de Lyon, CNRS and University of LyonEcole Normale Supérieure de Lyon, CNRS and University of LyonDepartment of Geology and Earth System Science Interdisciplinary Center (ESSIC), University of MarylandThe 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.https://doi.org/10.1038/s41467-019-08357-0 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
E. Gautier J. Savarino J. Hoek J. Erbland N. Caillon S. Hattori N. Yoshida E. Albalat F. Albarede J. Farquhar |
spellingShingle |
E. Gautier J. Savarino J. Hoek J. Erbland N. Caillon S. Hattori N. Yoshida E. Albalat F. Albarede J. Farquhar 2600-years of stratospheric volcanism through sulfate isotopes Nature Communications |
author_facet |
E. Gautier J. Savarino J. Hoek J. Erbland N. Caillon S. Hattori N. Yoshida E. Albalat F. Albarede J. Farquhar |
author_sort |
E. Gautier |
title |
2600-years of stratospheric volcanism through sulfate isotopes |
title_short |
2600-years of stratospheric volcanism through sulfate isotopes |
title_full |
2600-years of stratospheric volcanism through sulfate isotopes |
title_fullStr |
2600-years of stratospheric volcanism through sulfate isotopes |
title_full_unstemmed |
2600-years of stratospheric volcanism through sulfate isotopes |
title_sort |
2600-years of stratospheric volcanism through sulfate isotopes |
publisher |
Nature Publishing Group |
series |
Nature Communications |
issn |
2041-1723 |
publishDate |
2019-01-01 |
description |
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. |
url |
https://doi.org/10.1038/s41467-019-08357-0 |
work_keys_str_mv |
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