Articles | Volume 14, issue 10
Clim. Past, 14, 1405–1415, 2018
https://doi.org/10.5194/cp-14-1405-2018
Clim. Past, 14, 1405–1415, 2018
https://doi.org/10.5194/cp-14-1405-2018

Research article 08 Oct 2018

Research article | 08 Oct 2018

Ice core evidence for decoupling between midlatitude atmospheric water cycle and Greenland temperature during the last deglaciation

Amaëlle Landais et al.

Viewed

Total article views: 2,530 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,672 795 63 2,530 302 55 78
  • HTML: 1,672
  • PDF: 795
  • XML: 63
  • Total: 2,530
  • Supplement: 302
  • BibTeX: 55
  • EndNote: 78
Views and downloads (calculated since 14 Jun 2018)
Cumulative views and downloads (calculated since 14 Jun 2018)

Viewed (geographical distribution)

Total article views: 2,385 (including HTML, PDF, and XML) Thereof 2,353 with geography defined and 32 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 30 Jul 2021
Download
Short summary
During the last glacial–interglacial climate transition (120 000 to 10 000 years before present), Greenland climate and midlatitude North Atlantic climate and water cycle vary in phase over the succession of millennial events. We identify here one notable exception to this behavior with a decoupling unambiguously identified through a combination of water isotopic tracers measured in a Greenland ice core. The midlatitude moisture source becomes warmer and wetter at 16 200 years before present.