Articles | Volume 21, issue 3
https://doi.org/10.5194/cp-21-627-2025
https://doi.org/10.5194/cp-21-627-2025
Research article
 | 
11 Mar 2025
Research article |  | 11 Mar 2025

Patterns of changing surface climate variability from the Last Glacial Maximum to present in transient model simulations

Elisa Ziegler, Nils Weitzel, Jean-Philippe Baudouin, Marie-Luise Kapsch, Uwe Mikolajewicz, Lauren Gregoire, Ruza Ivanovic, Paul J. Valdes, Christian Wirths, and Kira Rehfeld

Viewed

Total article views: 758 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
565 151 42 758 58 25 27
  • HTML: 565
  • PDF: 151
  • XML: 42
  • Total: 758
  • Supplement: 58
  • BibTeX: 25
  • EndNote: 27
Views and downloads (calculated since 30 May 2024)
Cumulative views and downloads (calculated since 30 May 2024)

Viewed (geographical distribution)

Total article views: 758 (including HTML, PDF, and XML) Thereof 758 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 12 Mar 2025
Download
Short summary
During the Last Deglaciation, global surface temperature rose by about 4–7 °C over several millennia. We show that changes in year-to-year up to century-to-century fluctuations of temperature and precipitation during the Deglaciation were mostly larger than during either the preceding or succeeding more stable periods in 15 climate model simulations. The analysis demonstrates how ice sheets, meltwater, and volcanism influence simulated variability to inform future simulation protocols.
Share