Articles | Volume 21, issue 6
https://doi.org/10.5194/cp-21-1061-2025
https://doi.org/10.5194/cp-21-1061-2025
Research article
 | 
24 Jun 2025
Research article |  | 24 Jun 2025

CO2 and summer insolation as drivers for the Mid-Pleistocene Transition

Meike D. W. Scherrenberg, Constantijn J. Berends, and Roderik S. W. van de Wal

Viewed

Total article views: 1,720 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,200 392 128 1,720 56 80 115
  • HTML: 1,200
  • PDF: 392
  • XML: 128
  • Total: 1,720
  • Supplement: 56
  • BibTeX: 80
  • EndNote: 115
Views and downloads (calculated since 22 Aug 2024)
Cumulative views and downloads (calculated since 22 Aug 2024)

Viewed (geographical distribution)

Total article views: 1,720 (including HTML, PDF, and XML) Thereof 1,695 with geography defined and 25 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 16 Jan 2026
Short summary
Glacial cycle duration changed from 41 000 to 100 000 years during the Mid-Pleistocene Transition (MPT), but the cause is still under debate. We simulate the MPT with an ice sheet model forced by prescribed CO2 and insolation and simple ice–climate interactions. Before the MPT, glacial cycles follow insolation. After the MPT, low CO2 levels may compensate for warming at insolation maxima, increasing the length of glacial cycles until the North American ice sheet becomes large and thereby unstable.
Share