Articles | Volume 18, issue 3
https://doi.org/10.5194/tc-18-1381-2024
https://doi.org/10.5194/tc-18-1381-2024
Research article
 | 
26 Mar 2024
Research article |  | 26 Mar 2024

Modeling the timing of Patagonian Ice Sheet retreat in the Chilean Lake District from 22–10 ka

Joshua Cuzzone, Matias Romero, and Shaun A. Marcott

Viewed

Total article views: 1,250 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
880 318 52 1,250 21 40 46
  • HTML: 880
  • PDF: 318
  • XML: 52
  • Total: 1,250
  • Supplement: 21
  • BibTeX: 40
  • EndNote: 46
Views and downloads (calculated since 08 May 2023)
Cumulative views and downloads (calculated since 08 May 2023)

Viewed (geographical distribution)

Total article views: 1,250 (including HTML, PDF, and XML) Thereof 1,226 with geography defined and 24 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 08 May 2024
Download
Short summary
We simulate the retreat history of the Patagonian Ice Sheet (PIS) across the Chilean Lake District from 22–10 ka. These results improve our understanding of the response of the PIS to deglacial warming and the patterns of deglacial ice margin retreat where gaps in the geologic record still exist, and they indicate that changes in large-scale precipitation during the last deglaciation played an important role in modulating the response of ice margin change across the PIS to deglacial warming.