Articles | Volume 12, issue 3
https://doi.org/10.5194/cp-12-677-2016
© 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/cp-12-677-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Intra-interglacial climate variability: model simulations of Marine Isotope Stages 1, 5, 11, 13, and 15
Rima Rachmayani
CORRESPONDING AUTHOR
Faculty of Geosciences, University of Bremen, Klagenfurter
Straße, 28334 Bremen, Germany
Matthias Prange
Faculty of Geosciences, University of Bremen, Klagenfurter
Straße, 28334 Bremen, Germany
MARUM – Center for Marine
Environmental Sciences, University of Bremen, Leobener Straße, 28359 Bremen,
Germany
Michael Schulz
Faculty of Geosciences, University of Bremen, Klagenfurter
Straße, 28334 Bremen, Germany
MARUM – Center for Marine
Environmental Sciences, University of Bremen, Leobener Straße, 28359 Bremen,
Germany
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- Coupled climate-ice sheet modelling of MIS-13 reveals a sensitive Cordilleran Ice Sheet L. Niu et al. 10.1016/j.gloplacha.2021.103474
- Marine Isotope Stage 11c: An unusual interglacial P. Tzedakis et al. 10.1016/j.quascirev.2022.107493
- Pleistocene drivers of Northwest African hydroclimate and vegetation N. O’Mara et al. 10.1038/s41467-022-31120-x
- Sensitivity of the Greenland Ice Sheet to Interglacial Climate Forcing: MIS 5e Versus MIS 11 R. Rachmayani et al. 10.1002/2017PA003149
- Transient simulations of the present and the last interglacial climate using the Community Climate System Model version 3: effects of orbital acceleration V. Varma et al. 10.5194/gmd-9-3859-2016
- Simulating Marine Isotope Stage 7 with a coupled climate–ice sheet model D. Choudhury et al. 10.5194/cp-16-2183-2020
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- Sensitivity of the Antarctic ice sheets to the warming of marine isotope substage 11c M. Mas e Braga et al. 10.5194/tc-15-459-2021
- Obliquity-driven subtropical forcing of the thermocline after 240 ka in the southern sector of the Western Pacific Warm Pool J. Lambert et al. 10.1016/j.palaeo.2023.111578
- The global monsoon across time scales: Mechanisms and outstanding issues P. Wang et al. 10.1016/j.earscirev.2017.07.006
- Comparison of the green-to-desert Sahara transitions between the Holocene and the last interglacial H. Li et al. 10.5194/cp-18-2303-2022
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- Response of the Asian summer monsoons to idealized precession and obliquity forcing in a set of GCMs J. Bosmans et al. 10.1016/j.quascirev.2018.03.025
- Relative influence of precession and obliquity in the early Holocene: Topographic modulation of subtropical seasonality during the Asian summer monsoon C. Wu et al. 10.1016/j.quascirev.2018.05.021
- 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
- Precessional hydroclimatic synchronicity changes in the Indo-Pacific Warm Pool driven by the intertropical convergence zone over the past 450 kyr F. Qian et al. 10.1017/S0016756824000177
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Short summary
A set of 13 interglacial time slice experiments was carried out using a CCSM3-DGVM to study global climate variability between and within the Quaternary interglaciations of MIS 1, 5, 11, 13, and 15. Seasonal surface temperature anomalies can be explained by local insolation anomalies induced by the astronomical forcing in most regions and by GHG forcing at high latitudes and early Bruhnes interglacials. However, climate feedbacks may modify the surface temperature response in specific regions.
A set of 13 interglacial time slice experiments was carried out using a CCSM3-DGVM to study...