Articles | Volume 10, issue 4
https://doi.org/10.5194/cp-10-1305-2014
https://doi.org/10.5194/cp-10-1305-2014
Research article
 | 
10 Jul 2014
Research article |  | 10 Jul 2014

Simulating last interglacial climate with NorESM: role of insolation and greenhouse gases in the timing of peak warmth

P.M. Langebroek and K. H. Nisancioglu

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Cited articles

Andersson, C.,Risebrobakken, B., Jansen, E., and Dahl, S. O.: Late Holocene surface ocean conditions of the Norwegian Sea (Vøring Plateau), Paleoceanography, 18, 1044, https://doi.org/10.1029/2001PA000654, 2003.
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Bentsen, M., Bethke, I., Debernard, J. B., Iversen, T., Kirkevåg, A., Seland, Ø., Drange, H., Roelandt, C., Seierstad, I. A., Hoose, C., and Kristjánsson, J. E.: The Norwegian Earth System Model, NorESM1-M – Part 1: Description and basic evaluation of the physical climate, Geosci. Model Dev., 6, 687–720, https://doi.org/10.5194/gmd-6-687-2013, 2013.
Berger, A. L.: Long term variations of caloric insolation resulting from the Earth's orbital elements, Quaternary Res., 9, 139–167, 1978.
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