Articles | Volume 15, issue 5
https://doi.org/10.5194/cp-15-1757-2019
https://doi.org/10.5194/cp-15-1757-2019
Research article
 | 
16 Sep 2019
Research article |  | 16 Sep 2019

Enhanced Mediterranean water cycle explains increased humidity during MIS 3 in North Africa

Mike Rogerson, Yuri Dublyansky, Dirk L. Hoffmann, Marc Luetscher, Paul Töchterle, and Christoph Spötl

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
ED: Reconsider after major revisions (18 Feb 2019) by Dominik Fleitmann
AR by Michael Rogerson on behalf of the Authors (02 Apr 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (15 May 2019) by Dominik Fleitmann
RR by Anonymous Referee #1 (27 May 2019)
RR by Anonymous Referee #2 (14 Jun 2019)
ED: Publish subject to technical corrections (08 Jul 2019) by Dominik Fleitmann
AR by Michael Rogerson on behalf of the Authors (12 Jul 2019)  Author's response   Manuscript 
Download
Short summary
Rainfall in North Africa is known to vary through time and is likely to change as global climate warms. Here, we provide a new level of understanding about past rainfall in North Africa by looking at a stalagmite which formed within northeastern Libya between 67 and 30 thousand years ago. We find that at times more rain falls, and the associated moisture is mostly derived from the western Mediterranean during winter storms. Sometimes, water comes from the eastern Mediterranean.