Synchronizing the Greenland ice core and radiocarbon timescales over the  Holocene &ndash; Bayesian wiggle-matching of cosmogenic radionuclide records

Adolphi, F.; Muscheler, R.

doi:https://doi.org/10.5194/cp-12-15-2016

Articles | Volume 12, issue 1

https://doi.org/10.5194/cp-12-15-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/cp-12-15-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 12, issue 1

Research article

|

15 Jan 2016

Research article |

| 15 Jan 2016

Synchronizing the Greenland ice core and radiocarbon timescales over the Holocene – Bayesian wiggle-matching of cosmogenic radionuclide records

F. Adolphi and R. Muscheler

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Final revised paper (published on 15 Jan 2016)
Supplement to the final revised paper
Preprint (discussion started on 09 Jul 2015)

Interactive discussion

Status: closed

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

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- Supplement

RC C1531: 'Review of F. Adolphi and R. Muscheler: “Synchronizing the Greenland ice core and radiocarbon timescales over the Holocene – Bayesian wiggle-matching of cosmogenic radionuclide records”', Anonymous Referee #1, 31 Aug 2015
RC C1917: 'Review of Adolphi and Muscheler, Climate of the Past Discussions, 11, 2933-2975', Anonymous Referee #2, 07 Oct 2015
AC C2266: 'Response to referee comments', Florian Adolphi, 09 Nov 2015

Peer-review completion

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

ED: Publish subject to minor revisions (review by Editor) (04 Dec 2015) by Luke Skinner

AR by Florian Adolphi on behalf of the Authors (11 Dec 2015) Author's response Manuscript

ED: Publish as is (21 Dec 2015) by Luke Skinner

Short summary

Here we employ common variations in tree-ring ¹⁴C and Greenland ice core ¹⁰Be records to synchronize the Greenland ice core (GICC05) and the radiocarbon (IntCal13) timescale over the Holocene. We propose a transfer function between both timescales that allows continuous comparisons between radiocarbon dated and ice core climate records at unprecedented chronological precision.