Articles | Volume 19, issue 3
https://doi.org/10.5194/cp-19-637-2023
https://doi.org/10.5194/cp-19-637-2023
Research article
 | 
21 Mar 2023
Research article |  | 21 Mar 2023

How does the explicit treatment of convection alter the precipitation–soil hydrology interaction in the mid-Holocene African humid period?

Leonore Jungandreas, Cathy Hohenegger, and Martin Claussen

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Latest update: 13 Dec 2024
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Short summary
Increasing the vegetation cover over mid-Holcocene North Africa expands the West African monsoon ∼ 4–5° further north. This northward shift of monsoonal precipitation is caused by interactions of the land surface with large-scale monsoon circulation and the coupling of soil moisture to precipitation. We highlight the importance of considering not only how soil moisture influences precipitation but also how different precipitation characteristics alter the soil hydrology via runoff generation.