Articles | Volume 9, issue 11
https://doi.org/10.5194/gmd-9-3859-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-9-3859-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Transient simulations of the present and the last interglacial climate using the Community Climate System Model version 3: effects of orbital acceleration
MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
now at: National Institute of Water and Atmospheric Research, Wellington, New Zealand
Matthias Prange
MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
Faculty of Geosciences, University of Bremen, Bremen, Germany
Michael Schulz
MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
Faculty of Geosciences, University of Bremen, Bremen, Germany
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13 citations as recorded by crossref.
- Abrupt cold events in the North Atlantic Ocean in a transient Holocene simulation A. Klus et al. 10.5194/cp-14-1165-2018
- Spatial analysis of early-warning signals for a North Atlantic climate transition in a coupled GCM A. Klus et al. 10.1007/s00382-018-4567-7
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- Non-trivial role of internal climate feedback on interglacial temperature evolution X. Zhang & F. Chen 10.1038/s41586-021-03930-4
- Eurasian Holocene climate trends in transient coupled climate simulations and stable oxygen isotope records C. DANEK et al. 10.1002/jqs.3396
- Comparison of climate responses to orbital forcing at different latitudes during the Holocene Y. Jing et al. 10.1016/j.quaint.2022.02.004
- Dynamic boreal summer atmospheric circulation response as negative feedback to Greenland melt during the MIS-11 interglacial B. Crow et al. 10.5194/cp-18-775-2022
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Latest update: 09 Dec 2024
Short summary
We compare the results from simulations of the present and the last interglacial, with and without acceleration of the orbital forcing, using a comprehensive coupled climate model. In low latitudes, the simulation of long-term variations in interglacial surface climate is not significantly affected by the use of the acceleration technique and hence model–data comparison of surface variables is therefore not hampered but major repercussions of the orbital forcing are obvious below thermocline.
We compare the results from simulations of the present and the last interglacial, with and...