Articles | Volume 14, issue 10
https://doi.org/10.5194/cp-14-1405-2018
© Author(s) 2018. 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-14-1405-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
08 Oct 2018
Research article |
| 08 Oct 2018
| 08 Oct 2018
Ice core evidence for decoupling between midlatitude atmospheric water cycle and Greenland temperature during the last deglaciation
Amaëlle Landais
CORRESPONDING AUTHOR
Laboratoire des Sciences du Climat et de l'Environnement, IPSL, UMR
8212, CEA-CNRS-UVSQ-UPS, Gif sur Yvette, France
Emilie Capron
Centre for Ice and Climate, Niels Bohr Institute, University of
Copenhagen, Juliane Maries Vej 30, 2900, Copenhagen, Denmark
British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3
0ET, UK
Valérie Masson-Delmotte
Laboratoire des Sciences du Climat et de l'Environnement, IPSL, UMR
8212, CEA-CNRS-UVSQ-UPS, Gif sur Yvette, France
Samuel Toucanne
IFREMER, Laboratoire Géophysique et enregistrement
Sédimentaire, CS 10070, 29280 Plouzané, France
Rachael Rhodes
Department of Earth Sciences, University of Cambridge, Downing
Street, Cambridge, CB2 3EQ, UK
Trevor Popp
Centre for Ice and Climate, Niels Bohr Institute, University of
Copenhagen, Juliane Maries Vej 30, 2900, Copenhagen, Denmark
Bo Vinther
Centre for Ice and Climate, Niels Bohr Institute, University of
Copenhagen, Juliane Maries Vej 30, 2900, Copenhagen, Denmark
Bénédicte Minster
Laboratoire des Sciences du Climat et de l'Environnement, IPSL, UMR
8212, CEA-CNRS-UVSQ-UPS, Gif sur Yvette, France
Frédéric Prié
Laboratoire des Sciences du Climat et de l'Environnement, IPSL, UMR
8212, CEA-CNRS-UVSQ-UPS, Gif sur Yvette, France
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25 citations as recorded by crossref.
- Abrupt Heinrich Stadial 1 cooling missing in Greenland oxygen isotopes C. He et al. 10.1126/sciadv.abh1007
- Challenges in the Direct Determination of 17Oexcess in Microliter Amount of Water Extracted From Speleothem Fluid Inclusions S. Affolter & M. Leuenberger 10.3389/feart.2021.612436
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- Environmental changes in the Fleuve Manche paleoriver drainage system (Western Europe) linked to North Atlantic sub-millennial climate variability across Heinrich Stadial 1: Palynological evidence from the Bay of Biscay A. Penaud et al. 10.1016/j.palaeo.2024.112512
- High precise dating on the variation of the Asian summer monsoon since 37 ka BP T. Li et al. 10.1038/s41598-021-88597-7
- Variations in Asian summer monsoon and hydroclimate during Heinrich stadials 4 revealed by stalagmite stable isotopes and trace elements Y. Wu et al. 10.1016/j.quascirev.2022.107869
- The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability S. Toucanne et al. 10.1029/2020PA004068
- Coupled atmosphere-ice-ocean dynamics during Heinrich Stadial 2 X. Dong et al. 10.1038/s41467-022-33583-4
- The Greenland spatial fingerprint of Dansgaard–Oeschger events in observations and models C. Buizert et al. 10.1073/pnas.2402637121
- Triple Oxygen Isotope Systematics in the Hydrologic Cycle J. Surma et al. 10.2138/rmg.2021.86.12
- Ice Core 17O Reveals Past Changes in Surface Air Temperatures and Stratosphere to Troposphere Mass Exchange P. Aggarwal et al. 10.3390/atmos14081268
- Triple Oxygen Isotopic Compositions of Ocean Water from the Mariana Trench Y. Lin et al. 10.1021/acsearthspacechem.1c00187
- East Asian monsoon changes early in the last deglaciation and insights into the interpretation of oxygen isotope changes in the Chinese stalagmite record Y. Liang et al. 10.1016/j.quascirev.2020.106699
- Synchronizing ice-core and U ∕ Th timescales in the Last Glacial Maximum using Hulu Cave 14C and new 10Be measurements from Greenland and Antarctica G. Sinnl et al. 10.5194/cp-19-1153-2023
- The response and sensitivity of deuterium and 17O excess parameters in precipitation to hydroclimate processes Z. Xia et al. 10.1016/j.earscirev.2023.104432
- Modelling water isotopologues (1H2H16O, 1H217O) in the coupled numerical climate model iLOVECLIM (version 1.1.5) T. Extier et al. 10.5194/gmd-17-2117-2024
- Water isotopes, climate variability, and the hydrological cycle: recent advances and new frontiers S. Dee et al. 10.1088/2752-5295/accbe1
- The anatomy of past abrupt warmings recorded in Greenland ice E. Capron et al. 10.1038/s41467-021-22241-w
- Two-phase structure of tropical hydroclimate during Heinrich Stadial 1 and its global implications J. Huang et al. 10.1016/j.quascirev.2019.105900
- Baffin Bay sea ice extent and synoptic moisture transport drive water vapor isotope (<i>δ</i><sup>18</sup>O, <i>δ</i><sup>2</sup>H, and deuterium excess) variability in coastal northwest Greenland P. Akers et al. 10.5194/acp-20-13929-2020
- Antarctic temperature and CO<sub>2</sub>: near-synchrony yet variable phasing during the last deglaciation J. Chowdhry Beeman et al. 10.5194/cp-15-913-2019
- Eurasian Ice Sheet collapse was a major source of Meltwater Pulse 1A 14,600 years ago J. Brendryen et al. 10.1038/s41561-020-0567-4
- OSL-dating of the Pleistocene-Holocene climatic transition in loess from China, Europe and North America, and evidence for accretionary pedogenesis D. Constantin et al. 10.1016/j.earscirev.2021.103769
- Centennial-millennial scale ocean-climate variability in the northeastern Atlantic across the last three terminations H. Singh et al. 10.1016/j.gloplacha.2023.104100
Latest update: 14 Dec 2024
Short summary
During the last glacial–interglacial climate transition (120 000 to 10 000 years before present), Greenland climate and midlatitude North Atlantic climate and water cycle vary in phase over the succession of millennial events. We identify here one notable exception to this behavior with a decoupling unambiguously identified through a combination of water isotopic tracers measured in a Greenland ice core. The midlatitude moisture source becomes warmer and wetter at 16 200 years before present.
During the last glacial–interglacial climate transition (120 000 to 10 000 years before...
