Articles | Volume 8, issue 2
https://doi.org/10.5194/cp-8-589-2012
© Author(s) 2012. This work is distributed under the Creative Commons Attribution 3.0 License.
Special issue:
Research article
| 
20 Mar 2012
Research article |
| 20 Mar 2012
Systematic study of the impact of fresh water fluxes on the glacial carbon cycle
Related subject area
Subject: Carbon Cycle | Archive: Modelling only | Timescale: Millenial/D-O
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The atmospheric bridge communicated the δ13C decline during the last deglaciation to the global upper ocean
Mysteriously high Δ14C of the glacial atmosphere: influence of 14C production and carbon cycle changes
Ocean carbon inventory under warmer climate conditions – the case of the Last Interglacial
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Barker, S., Diz, P., Vautravers, M. J., Pike, J., Knorr, G., Hall, I. R., and Broecker, W. S.: Interhemispheric {A}tlantic seesaw response during the last deglaciation, Nature, 457, 1097–1102, https://doi.org/10.1038/nature07770, 2009.
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Bond, G., Broecker, W., Johnsen, S., McManus, J., Labeyrie, L., Jouzel, J., and Bonani, G.: Correlations between climate records from North Atlantic sediments and Greenland ice, Nature, 365, 143–147, https://doi.org/10.1038/365143a0, 1993.
