Articles | Volume 12, issue 4
https://doi.org/10.5194/essd-12-3341-2020
https://doi.org/10.5194/essd-12-3341-2020
Data description paper
 | 
10 Dec 2020
Data description paper |  | 10 Dec 2020

A global mean sea surface temperature dataset for the Last Interglacial (129–116 ka) and contribution of thermal expansion to sea level change

Chris S. M. Turney, Richard T. Jones, Nicholas P. McKay, Erik van Sebille, Zoë A. Thomas, Claus-Dieter Hillenbrand, and Christopher J. Fogwill

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Christian Turney on behalf of the Authors (15 Oct 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (16 Oct 2020) by Giuseppe M.R. Manzella
AR by Christian Turney on behalf of the Authors (21 Oct 2020)  Author's response   Manuscript 
ED: Publish as is (23 Oct 2020) by Giuseppe M.R. Manzella
AR by Christian Turney on behalf of the Authors (23 Oct 2020)
Download
Short summary
The Last Interglacial (129–116 ka) experienced global temperatures and sea levels higher than today. The direct contribution of warmer conditions to global sea level (thermosteric) are uncertain. We report a global network of sea surface temperatures. We find mean global annual temperature anomalies of 0.2 ± 0.1˚C and an early maximum peak of 0.9 ± 0.1˚C. Our reconstruction suggests warmer waters contributed on average 0.08 ± 0.1 m and a peak contribution of 0.39 ± 0.1 m to global sea level.