- Abstract:
-
The shallow overturning circulation of the oceans transports heat from the tropics to the mid-latitudes. This overturning also influences the uptake and storage of anthropogenic carbon (Cant). We demonstrate this by quantifying the relative importance of ocean thermodynamics, circulation and biogeochemistry in a global biochemistry and circulation model. Almost 2/3 of the Cant ocean uptake enters via gas exchange in waters that are lighter than the base of the ventilated thermocline. However,...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Publisher's version
- Files:
-
-
(pdf, 891.7KB)
-
- Publisher copy:
- 10.1038/srep35473
-
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- Publisher:
- Nature Publishing Group Publisher's website
- Journal:
- Scientific Reports Journal website
- Volume:
- 6
- Chapter number:
- 35473
- Publication date:
- 2016-11-03
- Acceptance date:
- 2016-09-28
- DOI:
- EISSN:
-
2045-2322
- ISSN:
-
2045-2322
- Pubs id:
-
pubs:658022
- URN:
-
uri:c7dc4b0a-bc81-495d-b900-4133989a87d3
- UUID:
-
uuid:c7dc4b0a-bc81-495d-b900-4133989a87d3
- Local pid:
- pubs:658022
- Copyright holder:
- Iudicone et al.
- Copyright date:
- 2016
- Notes:
- © the Author(s). This work is licensed under a Creative Commons Attribution 4.0 International License.
Journal article
The formation of the ocean's anthropogenic carbon reservoir
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