Articles | Volume 12, issue 9
https://doi.org/10.5194/cp-12-1919-2016
© 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-12-1919-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Impact of meltwater on high-latitude early Last Interglacial climate
Emma J. Stone
CORRESPONDING AUTHOR
BRIDGE, School of Geographical Sciences, University of Bristol,
Bristol, UK
Emilie Capron
British Antarctic Survey, Cambridge, UK
Centre for ice and Climate, Niels Bohr Institute, University of
Copenhagen, Copenhagen, Denmark
Daniel J. Lunt
BRIDGE, School of Geographical Sciences, University of Bristol,
Bristol, UK
Antony J. Payne
BRIDGE, School of Geographical Sciences, University of Bristol,
Bristol, UK
Joy S. Singarayer
Department of Meteorology, University of Reading, Reading, UK
Paul J. Valdes
BRIDGE, School of Geographical Sciences, University of Bristol,
Bristol, UK
Eric W. Wolff
Department of Earth Sciences, University of Cambridge, Cambridge, UK
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- 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
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- CMIP6/PMIP4 simulations of the mid-Holocene and Last Interglacial using HadGEM3: comparison to the pre-industrial era, previous model versions and proxy data C. Williams et al. 10.5194/cp-16-1429-2020
- Simulating the Last Interglacial Greenland stable water isotope peak: The role of Arctic sea ice changes I. Malmierca-Vallet et al. 10.1016/j.quascirev.2018.07.027
- Recent advances on the dynamical representation and our understanding of the warmer‑than‑present last interglacial climate É. Capron et al. 10.4000/quaternaire.8029
- Palaeoenvironmental conditions during MIS 6/MIS 5 transition recorded in speleothems from the Tatra Mountains J. Pawlak et al. 10.1111/bor.12472
- Analysing the timing of peak warming and minimum winter sea-ice extent in the Southern Ocean during MIS 5e M. Chadwick et al. 10.1016/j.quascirev.2019.106134
- Regional and global sea-surface temperatures during the last interglaciation J. Hoffman et al. 10.1126/science.aai8464
- Stable isotope compositions of speleothems from the last interglacial – Spatial patterns of climate fluctuations in Europe A. Demény et al. 10.1016/j.quascirev.2017.02.012
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- Large-scale features of Last Interglacial climate: results from evaluating the <i>lig127k</i> simulations for the Coupled Model Intercomparison Project (CMIP6)–Paleoclimate Modeling Intercomparison Project (PMIP4) B. Otto-Bliesner et al. 10.5194/cp-17-63-2021
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- A computationally efficient depression-filling algorithm for digital elevation models, applied to proglacial lake drainage C. Berends & R. van de Wal 10.5194/gmd-9-4451-2016
- Tipping elements and amplified polar warming during the Last Interglacial Z. Thomas et al. 10.1016/j.quascirev.2020.106222
- Refining patterns of melt with forward stratigraphic models of stable Pleistocene coastlines P. Boyden et al. 10.5194/esurf-11-917-2023
- How does the Southern Ocean palaeoenvironment during Marine Isotope Stage 5e compare to the modern? M. Chadwick et al. 10.1016/j.marmicro.2021.102066
- 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
- Atmospheric and oceanic circulation altered by global mean sea-level rise Z. Zhang et al. 10.1038/s41561-023-01153-y
2 citations as recorded by crossref.
- Greenland Ice Sheet influence on Last Interglacial climate: global sensitivity studies performed with an atmosphere–ocean general circulation model M. Pfeiffer & G. Lohmann 10.5194/cp-12-1313-2016
- Simulating the 128‐ka Antarctic Climate Response to Northern Hemisphere Ice Sheet Melting Using the Isotope‐Enabled HadCM3 M. Holloway et al. 10.1029/2018GL079647
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Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
Climate models forced only with greenhouse gas concentrations and orbital parameters representative of the early Last Interglacial are unable to reproduce the observed colder-than-present temperatures in the North Atlantic and the warmer-than-present temperatures in the Southern Hemisphere. Using a climate model forced also with a freshwater amount derived from data representing melting from the remnant Northern Hemisphere ice sheets accounts for this response via the bipolar seesaw mechanism.
Climate models forced only with greenhouse gas concentrations and orbital parameters...