Climate evolution across the Mid-Brunhes Transition

Barth, Aaron M.; Clark, Peter U.; Bill, Nicholas S.; He, Feng; Pisias, Nicklas G.

doi:https://doi.org/10.5194/cp-14-2071-2018

Articles | Volume 14, issue 12

Clim. Past, 14, 2071–2087, 2018

https://doi.org/10.5194/cp-14-2071-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: “Global Challenges for our Common Future: a paleoscience perspective”...

Clim. Past, 14, 2071–2087, 2018

https://doi.org/10.5194/cp-14-2071-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 14, issue 12

Research article 21 Dec 2018

Research article | 21 Dec 2018

Climate evolution across the Mid-Brunhes Transition

Aaron M. Barth et al.

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Final revised paper (published on 21 Dec 2018)
Supplement to the final revised paper
Preprint (discussion started on 27 Mar 2018)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

SC1: 'Data Review Team Comment', PAGES Data Review Team, 29 Apr 2018
- AC1: 'Response to PAGES Data Review Team', Aaron Barth, 27 Sep 2018
RC1: 'Review of Barth et al.', Anonymous Referee #1, 01 Jun 2018
- AC4: 'Response to Reviewer 1', Aaron Barth, 01 Oct 2018
RC2: 'Review of Barth et al.,', Anonymous Referee #2, 23 Jul 2018
- AC3: 'Response to Reviewer 2', Aaron Barth, 27 Sep 2018
EC1: 'Final Response - Editorial Team', Robert Barnett, 01 Aug 2018
AC2: 'Response to Reviewer 1', Aaron Barth, 27 Sep 2018

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (review by editor) (25 Oct 2018) by Robert Barnett

AR by Anna Wenzel on behalf of the Authors (06 Nov 2018) Author's response Manuscript

ED: Publish as is (26 Nov 2018) by Robert Barnett

Short summary

Multiple components of the global climate system record a transition ~ 430 ka from lower- to higher-amplitude glacial cycles. Statistical analyses of globally distributed climate proxies show that a sequence of events including persistent Asian summer monsoons, weak glaciation, and reorganization of water masses preceded the transition to higher interglacial values for temperature, atmospheric greenhouse gases, and sea level.