Articles | Volume 12, issue 2
https://doi.org/10.5194/cp-12-171-2016
© 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-12-171-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Spatial and temporal oxygen isotope variability in northern Greenland – implications for a new climate record over the past millennium
S. Weißbach
CORRESPONDING AUTHOR
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar-
und Meeresforschung, Bremerhaven, Germany
A. Wegner
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar-
und Meeresforschung, Bremerhaven, Germany
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar-
und Meeresforschung, Potsdam, Germany
H. Oerter
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar-
und Meeresforschung, Bremerhaven, Germany
B. M. Vinther
Centre for Ice and Climate, Niels Bohr Institute,
University of Copenhagen, Copenhagen, Denmark
S. Kipfstuhl
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar-
und Meeresforschung, Bremerhaven, Germany
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Cited
20 citations as recorded by crossref.
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- Ice-nucleating particle concentrations of the past: insights from a 600-year-old Greenland ice core J. Schrod et al. 10.5194/acp-20-12459-2020
- Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years N. Rimbu et al. 10.1029/2022GL101500
- Sea ice and pollution-modulated changes in Greenland ice core methanesulfonate and bromine O. Maselli et al. 10.5194/cp-13-39-2017
- Accumulation Rates during 1311–2011 CE in North-Central Greenland Derived from Air-Borne Radar Data N. Karlsson et al. 10.3389/feart.2016.00097
- Modern temperatures in central–north Greenland warmest in past millennium M. Hörhold et al. 10.1038/s41586-022-05517-z
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- A portable lightweight in situ analysis (LISA) box for ice and snow analysis H. Kjær et al. 10.5194/tc-15-3719-2021
- Climate variability in the subarctic area for the last 2 millennia M. Nicolle et al. 10.5194/cp-14-101-2018
- Applying an isotope-enabled regional climate model over the Greenland ice sheet: effect of spatial resolution on model bias M. Breil et al. 10.5194/cp-17-1685-2021
- Glacier response to the Little Ice Age during the Neoglacial cooling in Greenland K. Kjær et al. 10.1016/j.earscirev.2022.103984
- Annually resolved North Atlantic marine climate over the last millennium D. Reynolds et al. 10.1038/ncomms13502
- Tracing the isotopic signatures of cryospheric water and establishing the altitude effect in Central Himalayas: A tool for cryospheric water partitioning N. Pant et al. 10.1016/j.jhydrol.2021.125983
- Decadal-to-centennial increases of volcanic aerosols from Iceland challenge the concept of a Medieval Quiet Period I. Gabriel et al. 10.1038/s43247-024-01350-6
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- Laser Ultrasound Observations of Mechanical Property Variations in Ice Cores T. Mikesell et al. 10.3390/geosciences7030047
- Surface accumulation in Northern Central Greenland during the last 300 years N. Karlsson et al. 10.1017/aog.2020.30
20 citations as recorded by crossref.
- Industrial-era decline in subarctic Atlantic productivity M. Osman et al. 10.1038/s41586-019-1181-8
- Spatio-temporal variability of Arctic summer temperatures over the past 2 millennia J. Werner et al. 10.5194/cp-14-527-2018
- Ice-nucleating particle concentrations of the past: insights from a 600-year-old Greenland ice core J. Schrod et al. 10.5194/acp-20-12459-2020
- Interdecadal Pacific Oscillation in Northern Greenland Dust Concentration Variability During the Last 400 Years N. Rimbu et al. 10.1029/2022GL101500
- Sea ice and pollution-modulated changes in Greenland ice core methanesulfonate and bromine O. Maselli et al. 10.5194/cp-13-39-2017
- Accumulation Rates during 1311–2011 CE in North-Central Greenland Derived from Air-Borne Radar Data N. Karlsson et al. 10.3389/feart.2016.00097
- Modern temperatures in central–north Greenland warmest in past millennium M. Hörhold et al. 10.1038/s41586-022-05517-z
- Methanesulfonic acid (MSA) migration in polar ice: data synthesis and theory M. Osman et al. 10.5194/tc-11-2439-2017
- Arctic hydroclimate variability during the last 2000 years: current understanding and research challenges H. Linderholm et al. 10.5194/cp-14-473-2018
- Fe2+ in ice cores as a new potential proxy to detect past volcanic eruptions F. Burgay et al. 10.1016/j.scitotenv.2018.11.075
- A portable lightweight in situ analysis (LISA) box for ice and snow analysis H. Kjær et al. 10.5194/tc-15-3719-2021
- Climate variability in the subarctic area for the last 2 millennia M. Nicolle et al. 10.5194/cp-14-101-2018
- Applying an isotope-enabled regional climate model over the Greenland ice sheet: effect of spatial resolution on model bias M. Breil et al. 10.5194/cp-17-1685-2021
- Glacier response to the Little Ice Age during the Neoglacial cooling in Greenland K. Kjær et al. 10.1016/j.earscirev.2022.103984
- Annually resolved North Atlantic marine climate over the last millennium D. Reynolds et al. 10.1038/ncomms13502
- Tracing the isotopic signatures of cryospheric water and establishing the altitude effect in Central Himalayas: A tool for cryospheric water partitioning N. Pant et al. 10.1016/j.jhydrol.2021.125983
- Decadal-to-centennial increases of volcanic aerosols from Iceland challenge the concept of a Medieval Quiet Period I. Gabriel et al. 10.1038/s43247-024-01350-6
- A representative density profile of the North Greenland snowpack C. Schaller et al. 10.5194/tc-10-1991-2016
- Laser Ultrasound Observations of Mechanical Property Variations in Ice Cores T. Mikesell et al. 10.3390/geosciences7030047
- Surface accumulation in Northern Central Greenland during the last 300 years N. Karlsson et al. 10.1017/aog.2020.30
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Latest update: 13 Dec 2024
Short summary
Based on a set of 12 intermediate deep ice cores, covering an area of about 200 000 km2, we studied the spatial and temporal d18O patterns of northern Greenland over the past millennium and found a strong east-west gradient related to the main ice divide. A stacked record with significantly reduced noise revealed distinct climate variations with a pronounced Little Ice Age and distinct warm events such as the Medieval Climate Anomaly, around AD 1420 and in the 20th century.
Based on a set of 12 intermediate deep ice cores, covering an area of about 200 000 km2, we...