Climate of the Past
Climate of the Past
CP
Articles | Volume 20, issue 8
Articles | Volume 20, issue 8
https://doi.org/10.5194/cp-20-1761-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-20-1761-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 8
Research article
 | 
12 Aug 2024
Research article |  | 12 Aug 2024

Late Pleistocene glacial terminations accelerated by proglacial lakes

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

Viewed

Total article views: 1,047 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
753 247 47 1,047 21 51 38
  • HTML: 753
  • PDF: 247
  • XML: 47
  • Total: 1,047
  • Supplement: 21
  • BibTeX: 51
  • EndNote: 38
Views and downloads (calculated since 03 Jul 2023)
Cumulative views and downloads (calculated since 03 Jul 2023)

Viewed (geographical distribution)

Total article views: 1,047 (including HTML, PDF, and XML) Thereof 1,035 with geography defined and 12 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 31 Aug 2024
Download
Short summary
During Late Pleistocene glacial cycles, the Eurasian and North American ice sheets grew and melted, resulting in over 100 m of sea-level change. Studying the melting of past ice sheets can improve our understanding of how ice sheets might respond in the future. In this study, we find that melting increases due to proglacial lakes forming at the margins of the ice sheets, primarily due to the reduced basal friction of floating ice. Furthermore, bedrock uplift rates can strongly influence melting.
Read more
Special issue
Icy landscapes of the past (CP/ESSD/ESurf/TC inter-journal...