Articles | Volume 16, issue 6
https://doi.org/10.5194/cp-16-2183-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-2183-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Simulating Marine Isotope Stage 7 with a coupled climate–ice sheet model
Dipayan Choudhury
CORRESPONDING AUTHOR
Center for Climate Physics, Institute for Basic Science (IBS), Busan 46241, South Korea
Pusan National University, Busan 46241, South Korea
Axel Timmermann
Center for Climate Physics, Institute for Basic Science (IBS), Busan 46241, South Korea
Pusan National University, Busan 46241, South Korea
Fabian Schloesser
International Pacific Research Center, University of Hawaii at Manoa, Honolulu, HI 96822, USA
Malte Heinemann
Institute of Geosciences, Kiel University, 24118, Kiel, Germany
David Pollard
Earth and Environmental Systems Institute, Pennsylvania State
University, University Park, Pennsylvania, 16802, USA
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- Climate and ice sheet evolutions from the last glacial maximum to the pre-industrial period with an ice-sheet–climate coupled model A. Quiquet et al. https://doi.org/10.5194/cp-17-2179-2021
- Synchronous Glacial Cycles in a Nonsmooth Conceptual Climate Model with Asymmetric Hemispheres A. Nadeau et al. https://doi.org/10.1137/21M1390098
- Toward generalized Milankovitch theory (GMT) A. Ganopolski https://doi.org/10.5194/cp-20-151-2024
- Last glacial inception trajectories for the Northern Hemisphere from coupled ice and climate modelling T. Bahadory et al. https://doi.org/10.5194/cp-17-397-2021
- Incision and rock uplift along the Lower Seine River since Marine Isotope Stage 8 D. Chourio‐Camacho et al. https://doi.org/10.1002/jqs.3640
- The response of the Southern ocean to Climatological iceberg freshwater forcing J. Zhang et al. https://doi.org/10.1007/s00382-025-07922-2
- On the Cause of the Mid‐Pleistocene Transition C. Berends et al. https://doi.org/10.1029/2020RG000727
- The Marine Isotopic Stage 7: a relic of the “41 ka world”? Perspectives from a global-scale sea-surface temperature synthesis E. Legrain et al. https://doi.org/10.5194/cp-22-1223-2026
- Climate tipping point interactions and cascades: a review N. Wunderling et al. https://doi.org/10.5194/esd-15-41-2024
- Perched Hydrologic Systems of the Monahans and the Kermit Dune Fields, Northern Chihuahuan Desert, West Texas, USA A. Fournier et al. https://doi.org/10.3390/w16223188
- Modelling past and future demography of silver fir forests affected by dieback through genomic and dendroecological timelines I. García-García et al. https://doi.org/10.1016/j.scitotenv.2025.180329
- Increased sensitivity of the Antarctic Ice Sheet to decreasing CO2 across the Mid-Pleistocene Transition K. Yun & A. Timmermann https://doi.org/10.1038/s41561-026-01979-2
- Diet and habitat of the late Middle Pleistocene mammals from the Casal de’ Pazzi site (Rome, Italy) using stable carbon and oxygen isotope ratios G. Briatico et al. https://doi.org/10.1016/j.quaint.2023.11.002
- Late Middle Pleistocene (MIS 10–6) glacial–interglacial records from loess–palaeosol and fluvial sequences from northern France: a cyclostratigraphic approach P. Antoine & N. Limondin‐Lozouet https://doi.org/10.1111/bor.12662
15 citations as recorded by crossref.
- A long postglacial rhyolitic activity of the Icelandic Krafla volcano during the Eemian: limited impact of glacio-isostasy B. Van Vliet-Lanoë et al. https://doi.org/10.1051/bsgf/2025020
- Climate and ice sheet evolutions from the last glacial maximum to the pre-industrial period with an ice-sheet–climate coupled model A. Quiquet et al. https://doi.org/10.5194/cp-17-2179-2021
- Synchronous Glacial Cycles in a Nonsmooth Conceptual Climate Model with Asymmetric Hemispheres A. Nadeau et al. https://doi.org/10.1137/21M1390098
- Toward generalized Milankovitch theory (GMT) A. Ganopolski https://doi.org/10.5194/cp-20-151-2024
- Last glacial inception trajectories for the Northern Hemisphere from coupled ice and climate modelling T. Bahadory et al. https://doi.org/10.5194/cp-17-397-2021
- Incision and rock uplift along the Lower Seine River since Marine Isotope Stage 8 D. Chourio‐Camacho et al. https://doi.org/10.1002/jqs.3640
- The response of the Southern ocean to Climatological iceberg freshwater forcing J. Zhang et al. https://doi.org/10.1007/s00382-025-07922-2
- On the Cause of the Mid‐Pleistocene Transition C. Berends et al. https://doi.org/10.1029/2020RG000727
- The Marine Isotopic Stage 7: a relic of the “41 ka world”? Perspectives from a global-scale sea-surface temperature synthesis E. Legrain et al. https://doi.org/10.5194/cp-22-1223-2026
- Climate tipping point interactions and cascades: a review N. Wunderling et al. https://doi.org/10.5194/esd-15-41-2024
- Perched Hydrologic Systems of the Monahans and the Kermit Dune Fields, Northern Chihuahuan Desert, West Texas, USA A. Fournier et al. https://doi.org/10.3390/w16223188
- Modelling past and future demography of silver fir forests affected by dieback through genomic and dendroecological timelines I. García-García et al. https://doi.org/10.1016/j.scitotenv.2025.180329
- Increased sensitivity of the Antarctic Ice Sheet to decreasing CO2 across the Mid-Pleistocene Transition K. Yun & A. Timmermann https://doi.org/10.1038/s41561-026-01979-2
- Diet and habitat of the late Middle Pleistocene mammals from the Casal de’ Pazzi site (Rome, Italy) using stable carbon and oxygen isotope ratios G. Briatico et al. https://doi.org/10.1016/j.quaint.2023.11.002
- Late Middle Pleistocene (MIS 10–6) glacial–interglacial records from loess–palaeosol and fluvial sequences from northern France: a cyclostratigraphic approach P. Antoine & N. Limondin‐Lozouet https://doi.org/10.1111/bor.12662
Saved (final revised paper)
Latest update: 03 Aug 2026
Short summary
Our study is the first study to conduct transient simulations over MIS 7, using a 3-D coupled climate–ice sheet model with interactive ice sheets in both hemispheres. We find glacial inceptions to be more sensitive to orbital variations, whereas glacial terminations need the concerted action of both orbital and CO2 forcings. We highlight the issue of multiple equilibria and an instability due to stationary-wave–topography feedback that can trigger unrealistic North American ice sheet growth.
Our study is the first study to conduct transient simulations over MIS 7, using a 3-D coupled...