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

Viewed

Total article views: 1,267 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
933 283 51 1,267 38 33
  • HTML: 933
  • PDF: 283
  • XML: 51
  • Total: 1,267
  • BibTeX: 38
  • EndNote: 33
Views and downloads (calculated since 19 Sep 2022)
Cumulative views and downloads (calculated since 19 Sep 2022)

Viewed (geographical distribution)

Total article views: 1,267 (including HTML, PDF, and XML) Thereof 1,225 with geography defined and 42 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Jun 2024
Download
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.