Journal cover Journal topic
Climate of the Past An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 3.174 IF 3.174
  • IF 5-year value: 3.841 IF 5-year 3.841
  • CiteScore value: 3.48 CiteScore 3.48
  • SNIP value: 1.078 SNIP 1.078
  • SJR value: 1.981 SJR 1.981
  • IPP value: 3.38 IPP 3.38
  • h5-index value: 42 h5-index 42
  • Scimago H index value: 58 Scimago H index 58
CP | Articles | Volume 14, issue 12
Clim. Past, 14, 2011-2036, 2018
https://doi.org/10.5194/cp-14-2011-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Clim. Past, 14, 2011-2036, 2018
https://doi.org/10.5194/cp-14-2011-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 18 Dec 2018

Research article | 18 Dec 2018

Long-term deglacial permafrost carbon dynamics in MPI-ESM

Thomas Schneider von Deimling et al.
Viewed  
Total article views: 938 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
770 151 17 938 19 14
  • HTML: 770
  • PDF: 151
  • XML: 17
  • Total: 938
  • BibTeX: 19
  • EndNote: 14
Views and downloads (calculated since 06 Jun 2018)
Cumulative views and downloads (calculated since 06 Jun 2018)
Viewed (geographical distribution)  
Total article views: 710 (including HTML, PDF, and XML) Thereof 706 with geography defined and 4 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Cited  
Saved (final revised paper)  
No saved metrics found.
Saved (discussion paper)  
No saved metrics found.
Discussed (final revised paper)  
Discussed (discussion paper)  
No discussed metrics found.
Latest update: 21 Jan 2019
Publications Copernicus
Download
Short summary
Past cold ice age temperatures and the subsequent warming towards the Holocene had large consequences for soil organic carbon (SOC) stored in perennially frozen grounds. Using an Earth system model we show how the spread in areas affected by permafrost have changed under deglacial warming, along with changes in SOC accumulation. Our model simulations suggest phases of circum-Arctic permafrost SOC gain and losses, with a net increase in SOC between the last glacial maximum and the pre-industrial.
Past cold ice age temperatures and the subsequent warming towards the Holocene had large...
Citation
Share