Articles | Volume 11, issue 1
https://doi.org/10.5194/esd-11-13-2020
Special issue:
https://doi.org/10.5194/esd-11-13-2020
ESD Ideas
 | Highlight paper
 | 
17 Jan 2020
ESD Ideas | Highlight paper |  | 17 Jan 2020

ESD Ideas: Why are glaciations slower than deglaciations?

Christine Ramadhin and Chuixiang Yi

Viewed

Total article views: 4,519 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,606 798 115 4,519 99 117
  • HTML: 3,606
  • PDF: 798
  • XML: 115
  • Total: 4,519
  • BibTeX: 99
  • EndNote: 117
Views and downloads (calculated since 18 Mar 2019)
Cumulative views and downloads (calculated since 18 Mar 2019)

Viewed (geographical distribution)

Total article views: 4,519 (including HTML, PDF, and XML) Thereof 3,991 with geography defined and 528 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 26 Dec 2024
Download
Short summary
Here we explore ancient climate transitions from warm periods to ice ages and from ice ages to warm periods of the last 400 000 years. The changeovers from warm to ice age conditions are slower than those from ice age to warm conditions. We propose the presence of strong negative sea–ice feedbacks may be responsible for slowing the transition from warm to full ice age conditions. By improving understanding of past abrupt changes, we may have improved knowledge of future system behavior.
Special issue
Altmetrics
Final-revised paper
Preprint