Articles | Volume 16, issue 1
Clim. Past, 16, 117–140, 2020
Clim. Past, 16, 117–140, 2020

Research article 15 Jan 2020

Research article | 15 Jan 2020

The end of the African humid period as seen by a transient comprehensive Earth system model simulation of the last 8000 years

Anne Dallmeyer et al.


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: Publish subject to minor revisions (review by editor) (29 Oct 2019) by Ran Feng
AR by Anne Dallmeyer on behalf of the Authors (30 Oct 2019)  Author's response    Manuscript
ED: Publish subject to technical corrections (15 Nov 2019) by Ran Feng
Short summary
We analyse the end of the African humid period (AHP) in a transient Holocene simulation performed with the comprehensive Earth system model MPI-ESM1.2. The model reproduces the time-transgressive end of the AHP evident in proxy data and indicates that changes in moisture can be attributed to the retreat of the summer monsoon and to changes in the extratropical troughs. The spatially varying impact of these systems imposes regionally different responses to the Holocene insolation change.