Articles | Volume 7, issue 2
https://doi.org/10.5194/esd-7-295-2016
https://doi.org/10.5194/esd-7-295-2016
Research article
 | 
07 Apr 2016
Research article |  | 07 Apr 2016

The Southern Ocean as a constraint to reduce uncertainty in future ocean carbon sinks

A. Kessler and J. Tjiputra

Viewed

Total article views: 3,686 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,122 1,342 222 3,686 146 160
  • HTML: 2,122
  • PDF: 1,342
  • XML: 222
  • Total: 3,686
  • BibTeX: 146
  • EndNote: 160
Views and downloads (calculated since 21 Dec 2015)
Cumulative views and downloads (calculated since 21 Dec 2015)

Cited

Saved (final revised paper)

Latest update: 14 Dec 2024
Download
Short summary
The uncertainty of ocean carbon uptake in ESMs is projected to grow 2-fold by the end of the 21st century. We found that models that take up anomalously low (high) CO2 in the Southern Ocean (SO) today project low (high) cumulative CO2 uptake in the 21st century; thus the SO can be used to constrain future global uptake uncertainty. Inter-model spread in the SO carbon sink arises from variations in the pCO2 seasonality, specifically bias in the simulated timing and amplitude of NPP and SST.
Altmetrics
Final-revised paper
Preprint