Articles | Volume 11, issue 10
https://doi.org/10.5194/cp-11-1271-2015
© Author(s) 2015. 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-11-1271-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
01 Oct 2015
Research article |
| 01 Oct 2015
Orbital control on late Miocene climate and the North African monsoon: insight from an ensemble of sub-precessional simulations
A. Marzocchi
CORRESPONDING AUTHOR
School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol, UK
D. J. Lunt
School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol, UK
R. Flecker
School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol, UK
C. D. Bradshaw
Geophysical Institute, University of Bergen and Bjerknes Centre for Climate Research, Allégaten, Bergen, Norway
A. Farnsworth
School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol, UK
F. J. Hilgen
Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Budapestlaan 4, Utrecht, the Netherlands
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- Modes of Pangean lake level cyclicity driven by astronomical climate pacing modulated by continental position and p CO2 J. Landwehrs et al. 10.1073/pnas.2203818119
- Mediterranean isolation preconditioning the Earth System for late Miocene climate cooling W. Capella et al. 10.1038/s41598-019-40208-2
- Indian monsoon variability in response to orbital forcing during the late Pliocene C. Prescott et al. 10.1016/j.gloplacha.2018.12.002
- Climate stability in central Anatolia during the Messinian Salinity Crisis M. Meijers et al. 10.1016/j.palaeo.2018.03.001
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- Investigating Sensitivity of East Asian Monsoon to Orbital Forcing During the Late Pliocene Warm Period Q. Yan et al. 10.1029/2017JD027646
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Short summary
This paper investigates the climatic response to orbital forcing through the analysis of an ensemble of simulations covering a late Miocene precession cycle. Including orbital variability in our model–data comparison reduces the mismatch between the proxy record and model output. Our results indicate that ignoring orbital variability could lead to miscorrelations in proxy reconstructions. The North African summer monsoon's sensitivity is high to orbits, moderate to paleogeography and low to CO2.
This paper investigates the climatic response to orbital forcing through the analysis of an...
