Articles | Volume 12, issue 8
Clim. Past, 12, 1721–1737, 2016
https://doi.org/10.5194/cp-12-1721-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Clim. Past, 12, 1721–1737, 2016
https://doi.org/10.5194/cp-12-1721-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article 25 Aug 2016
Research article | 25 Aug 2016
Impact of ice sheet meltwater fluxes on the climate evolution at the onset of the Last Interglacial
Heiko Goelzer et al.
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Cited
10 citations as recorded by crossref.
- Impact of meltwater on high-latitude early Last Interglacial climate E. Stone et al. 10.5194/cp-12-1919-2016
- The PMIP4 contribution to CMIP6 – Part 2: Two interglacials, scientific objective and experimental design for Holocene and Last Interglacial simulations B. Otto-Bliesner et al. 10.5194/gmd-10-3979-2017
- Semi-equilibrated global sea-level change projections for the next 10 000 years J. Van Breedam et al. 10.5194/esd-11-953-2020
- The penultimate deglaciation: protocol for Paleoclimate Modelling Intercomparison Project (PMIP) phase 4 transient numerical simulations between 140 and 127 ka, version 1.0 L. Menviel et al. 10.5194/gmd-12-3649-2019
- Last Interglacial climate and sea-level evolution from a coupled ice sheet–climate model H. Goelzer et al. 10.5194/cp-12-2195-2016
- Dynamic Greenland ice sheet driven by pCO2 variations across the Pliocene Pleistocene transition N. Tan et al. 10.1038/s41467-018-07206-w
- Critical evaluation of climate syntheses to benchmark CMIP6/PMIP4 127 ka Last Interglacial simulations in the high-latitude regions E. Capron et al. 10.1016/j.quascirev.2017.04.019
- Recent Progress in Greenland Ice Sheet Modelling H. Goelzer et al. 10.1007/s40641-017-0073-y
- A new approach for simulating the paleo-evolution of the Northern Hemisphere ice sheets R. Banderas et al. 10.5194/gmd-11-2299-2018
- Paleoclimate in continental northwestern Europe during the Eemian and early Weichselian (125–97 ka): insights from a Belgian speleothem S. Vansteenberge et al. 10.5194/cp-12-1445-2016
9 citations as recorded by crossref.
- Impact of meltwater on high-latitude early Last Interglacial climate E. Stone et al. 10.5194/cp-12-1919-2016
- The PMIP4 contribution to CMIP6 – Part 2: Two interglacials, scientific objective and experimental design for Holocene and Last Interglacial simulations B. Otto-Bliesner et al. 10.5194/gmd-10-3979-2017
- Semi-equilibrated global sea-level change projections for the next 10 000 years J. Van Breedam et al. 10.5194/esd-11-953-2020
- The penultimate deglaciation: protocol for Paleoclimate Modelling Intercomparison Project (PMIP) phase 4 transient numerical simulations between 140 and 127 ka, version 1.0 L. Menviel et al. 10.5194/gmd-12-3649-2019
- Last Interglacial climate and sea-level evolution from a coupled ice sheet–climate model H. Goelzer et al. 10.5194/cp-12-2195-2016
- Dynamic Greenland ice sheet driven by pCO2 variations across the Pliocene Pleistocene transition N. Tan et al. 10.1038/s41467-018-07206-w
- Critical evaluation of climate syntheses to benchmark CMIP6/PMIP4 127 ka Last Interglacial simulations in the high-latitude regions E. Capron et al. 10.1016/j.quascirev.2017.04.019
- Recent Progress in Greenland Ice Sheet Modelling H. Goelzer et al. 10.1007/s40641-017-0073-y
- A new approach for simulating the paleo-evolution of the Northern Hemisphere ice sheets R. Banderas et al. 10.5194/gmd-11-2299-2018
Saved (preprint)
Latest update: 24 Jul 2021
Short summary
We have modelled the climate evolution from 135 to 120 kyr BP with an Earth system model to study the onset of the Last Interglacial warm period. Ice sheet changes and associated freshwater fluxes in both hemispheres constitute an important forcing in the simulations. Freshwater fluxes from the melting Antarctic ice sheet are found to lead to an oceanic cold event in the Southern Ocean as evidenced in some ocean sediment cores, which may be used to constrain the timing of ice sheet retreat.
We have modelled the climate evolution from 135 to 120 kyr BP with an Earth system model to...
