Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-117-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-117-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Jan 2020
Research article |
| 15 Jan 2020
| 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
CORRESPONDING AUTHOR
The Land in the Earth System, Max Planck Institute for Meteorology, Bundesstrasse 53, 20146 Hamburg, Germany
Martin Claussen
The Land in the Earth System, Max Planck Institute for Meteorology, Bundesstrasse 53, 20146 Hamburg, Germany
Meteorological Institute, Centrum für Erdsystemforschung und
Nachhaltigkeit (CEN), Universität Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany
Stephan J. Lorenz
The Ocean in the Earth System, Max Planck Institute for Meteorology, Bundesstrasse 53, 20146 Hamburg, Germany
Timothy Shanahan
The University of Texas at Austin, Department of Geological Sciences, 1 University Station C9000, Austin, Texas 78712, USA
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- Effects of orbital forcing, greenhouse gases and ice sheets on Saharan greening in past and future multi-millennia M. Duque-Villegas et al. 10.5194/cp-18-1897-2022
- نظرة عامة على المواقع السكنية للبليستوسين الأعلى في ليبيا، والصلات البين- ثقافية مع نظيراتها الصحراوية-الساحلية والشرق أبيضية المتوسطية. أ. الضبع 10.59743/jaf.v4i2.170
- Drivers of the evolution and amplitude of African Humid Periods L. Menviel et al. 10.1038/s43247-021-00309-1
- Atmospheric methane since the last glacial maximum was driven by wetland sources T. Kleinen et al. 10.5194/cp-19-1081-2023
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Latest update: 03 Jul 2025
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.
We analyse the end of the African humid period (AHP) in a transient Holocene simulation...
