Articles | Volume 14, issue 10
Clim. Past, 14, 1405–1415, 2018
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.
Clim. Past, 14, 1405–1415, 2018
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
Ice core evidence for decoupling between midlatitude atmospheric water cycle and Greenland temperature during the last deglaciation
Amaëlle Landais et al.
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Cited
12 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
- 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
- Hydroclimatic changes in the British Isles through the Last-Glacial-Interglacial Transition: Multiproxy reconstructions from the Vale of Pickering, NE England P. Lincoln et al. 10.1016/j.quascirev.2020.106630
- 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
- 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
- The anatomy of past abrupt warmings recorded in Greenland ice E. Capron et al. 10.1038/s41467-021-22241-w
- Triple Oxygen Isotope Systematics in the Hydrologic Cycle J. Surma et al. 10.2138/rmg.2021.86.12
- 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
12 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
- 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
- Hydroclimatic changes in the British Isles through the Last-Glacial-Interglacial Transition: Multiproxy reconstructions from the Vale of Pickering, NE England P. Lincoln et al. 10.1016/j.quascirev.2020.106630
- 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
- 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
- The anatomy of past abrupt warmings recorded in Greenland ice E. Capron et al. 10.1038/s41467-021-22241-w
- Triple Oxygen Isotope Systematics in the Hydrologic Cycle J. Surma et al. 10.2138/rmg.2021.86.12
- 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
Latest update: 30 Jul 2021
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...
