Journal cover Journal topic
Earth System Dynamics An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 3.866 IF 3.866
  • IF 5-year value: 4.135 IF 5-year
    4.135
  • CiteScore value: 7.0 CiteScore
    7.0
  • SNIP value: 1.182 SNIP 1.182
  • IPP value: 3.86 IPP 3.86
  • SJR value: 1.883 SJR 1.883
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 33 Scimago H
    index 33
  • h5-index value: 30 h5-index 30
ESD | Articles | Volume 11, issue 1
Earth Syst. Dynam., 11, 13–16, 2020
https://doi.org/10.5194/esd-11-13-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: ESD Ideas

Earth Syst. Dynam., 11, 13–16, 2020
https://doi.org/10.5194/esd-11-13-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

ESD Ideas 17 Jan 2020

ESD Ideas | 17 Jan 2020

ESD Ideas: Why are glaciations slower than deglaciations?

Christine Ramadhin and Chuixiang Yi

Viewed

Total article views: 1,702 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,364 302 36 1,702 44 56
  • HTML: 1,364
  • PDF: 302
  • XML: 36
  • Total: 1,702
  • BibTeX: 44
  • EndNote: 56
Views and downloads (calculated since 18 Mar 2019)
Cumulative views and downloads (calculated since 18 Mar 2019)

Viewed (geographical distribution)

Total article views: 1,408 (including HTML, PDF, and XML) Thereof 1,405 with geography defined and 3 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

No saved metrics found.

Saved (preprint)

No saved metrics found.

Discussed (final revised paper)

No discussed metrics found.

Discussed (preprint)

No discussed metrics found.
Latest update: 04 Aug 2020
Publications Copernicus
Special issue
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.
Here we explore ancient climate transitions from warm periods to ice ages and from ice ages to...
Citation
Final-revised paper
Preprint