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Clim. Past, 14, 811-824, 2018
https://doi.org/10.5194/cp-14-811-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Research article
18 Jun 2018
Assessing the impact of large volcanic eruptions of the last millennium (850–1850 CE) on Australian rainfall regimes
Stephanie A. P. Blake et al.
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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Review Comments for Blake et al.', Anonymous Referee #1, 03 Oct 2017 Printer-friendly Version 
AC1: 'Reply to Reviwer 1', Stephanie Blake, 04 Dec 2017 Printer-friendly Version 
 
RC2: 'Comment on “Assessing the impact of large volcanic eruptions of the Last Millennium on Australian rainfall regimes ” by Blake et al', Anonymous Referee #2, 12 Oct 2017 Printer-friendly Version Supplement 
AC2: 'Reply to Reviewer 2', Stephanie Blake, 04 Dec 2017 Printer-friendly Version 
 
SC1: 'Review of ‘Assessing the impact of large volcanic eruptions of the Last Millenium on Australian rainfall regimes’ by Blake et al.', Marte Stoorvogel, 04 Nov 2017 Printer-friendly Version Supplement 
AC3: 'Reply to Reviewer 3', Stephanie Blake, 04 Dec 2017 Printer-friendly Version 
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (11 Dec 2017) by Stefan Bronnimann  
AR by Anna Wenzel on behalf of the Authors (01 Mar 2018)  Author's response  Manuscript
ED: Referee Nomination & Report Request started (07 Mar 2018) by Stefan Bronnimann
RR by Anonymous Referee #1 (13 Mar 2018)  
RR by Anonymous Referee #2 (28 Mar 2018)  
ED: Publish subject to minor revisions (review by editor) (17 Apr 2018) by Stefan Bronnimann  
AR by Stephanie Blake on behalf of the Authors (10 May 2018)  Author's response  Manuscript
ED: Publish as is (17 May 2018) by Stefan Bronnimann  
CC BY 4.0
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Short summary
We studied the impact of the six largest tropical eruptions in reference to Australian precipitation, the Indian Ocean Dipole (IOD), and El Niño–Southern Oscillation (ENSO). Volcanic forcing increased the likelihood of El Niños and positive IODs (pIOD) and caused positive rainfall anomalies over north-west (NW) and south-east (SE) Australia. Larger sulfate loading caused more persistent pIOD and El Niños, enhanced precipitation over NW Australia, and dampened precipitation over SE Australia.
We studied the impact of the six largest tropical eruptions in reference to Australian...
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