Articles | Volume 13, issue 3
https://doi.org/10.5194/cp-13-201-2017
https://doi.org/10.5194/cp-13-201-2017
Research article
 | 
09 Mar 2017
Research article |  | 09 Mar 2017

Changes in Holocene meridional circulation and poleward Atlantic flow: the Bay of Biscay as a nodal point

Yannick Mary, Frédérique Eynaud, Christophe Colin, Linda Rossignol, Sandra Brocheray, Meryem Mojtahid, Jennifer Garcia, Marion Peral, Hélène Howa, Sébastien Zaragosi, and Michel Cremer

Viewed

Total article views: 3,058 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,734 1,136 188 3,058 470 117 168
  • HTML: 1,734
  • PDF: 1,136
  • XML: 188
  • Total: 3,058
  • Supplement: 470
  • BibTeX: 117
  • EndNote: 168
Views and downloads (calculated since 25 Apr 2016)
Cumulative views and downloads (calculated since 25 Apr 2016)

Cited

Saved (preprint)

Discussed (final revised paper)

Latest update: 28 Mar 2024
Download
Short summary
In the boreal Atlantic, the subpolar and subtropical gyres (SPG and STG respectively) are key elements of the Atlantic Meridional Overturning Circulation (AMOC) cell and contribute to climate modulations over Europe. Here we document the last 10 kyr evolution of sea-surface temperatures over the North Atlantic with a focus on new data obtained from an exceptional sedimentary archive retrieved the southern Bay of Biscay, enabling the study of Holocene archives at (infra)centennial scales.