Articles | Volume 16, issue 4
https://doi.org/10.5194/cp-16-1369-2020
© 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-16-1369-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
31 Jul 2020
Research article |
| 31 Jul 2020
| 31 Jul 2020
High-frequency climate variability in the Holocene from a coastal-dome ice core in east-central Greenland
Abigail G. Hughes
CORRESPONDING AUTHOR
Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, Colorado, USA
Tyler R. Jones
Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, Colorado, USA
Bo M. Vinther
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark
Vasileios Gkinis
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark
C. Max Stevens
Department of Earth and Space Sciences, University of Washington, Seattle, Washington, USA
Valerie Morris
Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, Colorado, USA
Bruce H. Vaughn
Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, Colorado, USA
Christian Holme
Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark
Bradley R. Markle
Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, Colorado, USA
California Institute of Technology, Pasadena, California, USA
James W. C. White
Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, Colorado, USA
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Cited
12 citations as recorded by crossref.
- Continuous-Flow Analysis of δ17O, δ18O, and δD of H2O on an Ice Core from the South Pole E. Steig et al. 10.3389/feart.2021.640292
- Sublimation Origin of Negative Deuterium Excess Observed in Snow and Ice Samples From McMurdo Dry Valleys and Allan Hills Blue Ice Areas, East Antarctica J. Hu et al. 10.1029/2021JD035950
- Coccolithophore assemblage composition during the Greenland Interstadial–Stadial 20 transition and their response to the Youngest Toba Tuff (YTT) supereruption ∼74,000 years ago in the northeastern Arabian Sea J. Guballa et al. 10.1371/journal.pone.0310041
- Seasonally Resolved Holocene Sea Ice Variability Inferred From South Pole Ice Core Chemistry D. Winski et al. 10.1029/2020GL091602
- Sea ice in the northern North Atlantic through the Holocene: Evidence from ice cores and marine sediment records N. Maffezzoli et al. 10.1016/j.quascirev.2021.107249
- Calibration of Arctic ice core bromine enrichment records for past sea ice reconstructions F. Scoto et al. 10.1016/j.scitotenv.2024.177063
- The role of sublimation as a driver of climate signals in the water isotope content of surface snow: laboratory and field experimental results A. Hughes et al. 10.5194/tc-15-4949-2021
- Seasonal temperatures in West Antarctica during the Holocene T. Jones et al. 10.1038/s41586-022-05411-8
- An East Antarctic, sub-annual resolution water isotope record from the Mount Brown South Ice core V. Gkinis et al. 10.1038/s41597-024-03751-w
- Shifts in Greenland interannual climate variability lead Dansgaard–Oeschger abrupt warming by hundreds of years C. Brashear et al. 10.5194/cp-21-529-2025
- Five thousand years of fire history in the high North Atlantic region: natural variability and ancient human forcing D. Segato et al. 10.5194/cp-17-1533-2021
- The Community Firn Model (CFM) v1.0 C. Stevens et al. 10.5194/gmd-13-4355-2020
12 citations as recorded by crossref.
- Continuous-Flow Analysis of δ17O, δ18O, and δD of H2O on an Ice Core from the South Pole E. Steig et al. 10.3389/feart.2021.640292
- Sublimation Origin of Negative Deuterium Excess Observed in Snow and Ice Samples From McMurdo Dry Valleys and Allan Hills Blue Ice Areas, East Antarctica J. Hu et al. 10.1029/2021JD035950
- Coccolithophore assemblage composition during the Greenland Interstadial–Stadial 20 transition and their response to the Youngest Toba Tuff (YTT) supereruption ∼74,000 years ago in the northeastern Arabian Sea J. Guballa et al. 10.1371/journal.pone.0310041
- Seasonally Resolved Holocene Sea Ice Variability Inferred From South Pole Ice Core Chemistry D. Winski et al. 10.1029/2020GL091602
- Sea ice in the northern North Atlantic through the Holocene: Evidence from ice cores and marine sediment records N. Maffezzoli et al. 10.1016/j.quascirev.2021.107249
- Calibration of Arctic ice core bromine enrichment records for past sea ice reconstructions F. Scoto et al. 10.1016/j.scitotenv.2024.177063
- The role of sublimation as a driver of climate signals in the water isotope content of surface snow: laboratory and field experimental results A. Hughes et al. 10.5194/tc-15-4949-2021
- Seasonal temperatures in West Antarctica during the Holocene T. Jones et al. 10.1038/s41586-022-05411-8
- An East Antarctic, sub-annual resolution water isotope record from the Mount Brown South Ice core V. Gkinis et al. 10.1038/s41597-024-03751-w
- Shifts in Greenland interannual climate variability lead Dansgaard–Oeschger abrupt warming by hundreds of years C. Brashear et al. 10.5194/cp-21-529-2025
- Five thousand years of fire history in the high North Atlantic region: natural variability and ancient human forcing D. Segato et al. 10.5194/cp-17-1533-2021
- The Community Firn Model (CFM) v1.0 C. Stevens et al. 10.5194/gmd-13-4355-2020
Latest update: 23 Apr 2025
Short summary
An ice core drilled on the Renland ice cap (RECAP) in east-central Greenland contains a continuous climate record dating through the last glacial period. Here we present the water isotope record for the Holocene, in which high-resolution climate information is retained for the last 8 kyr. We find that the RECAP water isotope record exhibits seasonal and decadal variability which may reflect sea surface conditions and regional climate variability.
An ice core drilled on the Renland ice cap (RECAP) in east-central Greenland contains a...
