Articles | Volume 9, issue 4
https://doi.org/10.5194/cp-9-1629-2013
© Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License.
Research article
| 
29 Jul 2013
Research article |
| 29 Jul 2013
The Holocene thermal maximum in the Nordic Seas: the impact of Greenland Ice Sheet melt and other forcings in a coupled atmosphere–sea-ice–ocean model
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Cited articles
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Andersson, C., Pausata, F. S. R., Jansen, E., Risebrobakken, B., and Telford, R. J.: Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean, Clim. Past, 6, 179–193, https://doi.org/10.5194/cp-6-179-2010, 2010.
Bakker, P., Van Meerbeeck, C. J., and Renssen, H.: Sensitivity of the North Atlantic climate to Greenland Ice Sheet melting during the Last Interglacial, Clim. Past, 8, 995–1009, https://doi.org/10.5194/cp-8-995-2012, 2012.
Berger, A. and Loutre, M.: Insolation values for the climate of the last 10 million years, Quaternary Sci. Rev., 10, 297–317, https://doi.org/10.1016/0277-3791(91)90033-Q, 1991.
Brovkin, V., Bendtsen, J., Claussen, M., Ganopolski, A., Kubatzki, C., Petoukhov, V., and Andreev, A.: Carbon cycle, vegetation, and climate dynamics in the Holocene: Experiments with the CLIMBER-2 model, Global Biogeochem. Cy., 16, 86-1–86-20, https://doi.org/10.1029/2001GB001662, 2002.
