Articles | Volume 7, issue 1
https://doi.org/10.5194/cp-7-319-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-7-319-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
28 Mar 2011
Research article |
| 28 Mar 2011
Fingerprints of changes in the terrestrial carbon cycle in response to large reorganizations in ocean circulation
A. Bozbiyik
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
M. Steinacher
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
F. Joos
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
T. F. Stocker
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
L. Menviel
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
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45 citations as recorded by crossref.
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- Millennial-scale atmospheric CO<sub>2</sub> variations during the Marine Isotope Stage 6 period (190–135 ka) J. Shin et al. 10.5194/cp-16-2203-2020
- Glacial CO<sub>2</sub> cycle as a succession of key physical and biogeochemical processes V. Brovkin et al. 10.5194/cp-8-251-2012
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- Southern Ocean link between changes in atmospheric CO2 levels and northern-hemisphere climate anomalies during the last two glacial periods J. Gottschalk et al. 10.1016/j.quascirev.2019.106067
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- Exceeding 1.5°C global warming could trigger multiple climate tipping points D. Armstrong McKay et al. 10.1126/science.abn7950
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