50 year means of oxygen isotope data from ice core NGRIP ...

Two deep ice cores from central Greenland, drilled in the 1990s, have played a key role in climate reconstructions of the Northern Hemisphere, but the oldest sections of the cores were disturbed in chronology owing to ice folding near the bedrock. Here we present an undisturbed climate record from a...

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Bibliographic Details
Main Author: North Greenland Ice Core Project Members
Format: Dataset
Language:English
Published: PANGAEA 2007
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.586886
https://doi.pangaea.de/10.1594/PANGAEA.586886
id ftdatacite:10.1594/pangaea.586886
record_format openpolar
spelling ftdatacite:10.1594/pangaea.586886 2024-09-15T18:08:25+00:00 50 year means of oxygen isotope data from ice core NGRIP ... North Greenland Ice Core Project Members 2007 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.586886 https://doi.pangaea.de/10.1594/PANGAEA.586886 en eng PANGAEA https://dx.doi.org/10.1038/nature02805 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 AGE δ18O, water Ice drill NGRIP Sampling/drilling ice North Greenland Ice Core Project NGRIP dataset Supplementary Dataset Dataset 2007 ftdatacite https://doi.org/10.1594/pangaea.58688610.1038/nature02805 2024-08-01T11:00:37Z Two deep ice cores from central Greenland, drilled in the 1990s, have played a key role in climate reconstructions of the Northern Hemisphere, but the oldest sections of the cores were disturbed in chronology owing to ice folding near the bedrock. Here we present an undisturbed climate record from a North Greenland ice core, which extends back to 123,000 years before the present, within the last interglacial period. The oxygen isotopes in the ice imply that climate was stable during the last interglacial period, with temperatures 5 °C warmer than today. We find unexpectedly large temperature differences between our new record from northern Greenland and the undisturbed sections of the cores from central Greenland, suggesting that the extent of ice in the Northern Hemisphere modulated the latitudinal temperature gradients in Greenland. This record shows a slow decline in temperatures that marked the initiation of the last glacial period. Our record reveals a hitherto unrecognized warm period initiated by an ... : The initial isotope data series is based on 5 cm continuous sampling from surface to bottom of the core, or 61100 individual measurements. The age model follows the GRIP2001/ss09sea timescale (Johnsen et al., 2001) ... Dataset Greenland Greenland ice core Greenland Ice core Project ice core NGRIP North Greenland North Greenland Ice Core Project DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic AGE
δ18O, water
Ice drill
NGRIP
Sampling/drilling ice
North Greenland Ice Core Project NGRIP
spellingShingle AGE
δ18O, water
Ice drill
NGRIP
Sampling/drilling ice
North Greenland Ice Core Project NGRIP
North Greenland Ice Core Project Members
50 year means of oxygen isotope data from ice core NGRIP ...
topic_facet AGE
δ18O, water
Ice drill
NGRIP
Sampling/drilling ice
North Greenland Ice Core Project NGRIP
description Two deep ice cores from central Greenland, drilled in the 1990s, have played a key role in climate reconstructions of the Northern Hemisphere, but the oldest sections of the cores were disturbed in chronology owing to ice folding near the bedrock. Here we present an undisturbed climate record from a North Greenland ice core, which extends back to 123,000 years before the present, within the last interglacial period. The oxygen isotopes in the ice imply that climate was stable during the last interglacial period, with temperatures 5 °C warmer than today. We find unexpectedly large temperature differences between our new record from northern Greenland and the undisturbed sections of the cores from central Greenland, suggesting that the extent of ice in the Northern Hemisphere modulated the latitudinal temperature gradients in Greenland. This record shows a slow decline in temperatures that marked the initiation of the last glacial period. Our record reveals a hitherto unrecognized warm period initiated by an ... : The initial isotope data series is based on 5 cm continuous sampling from surface to bottom of the core, or 61100 individual measurements. The age model follows the GRIP2001/ss09sea timescale (Johnsen et al., 2001) ...
format Dataset
author North Greenland Ice Core Project Members
author_facet North Greenland Ice Core Project Members
author_sort North Greenland Ice Core Project Members
title 50 year means of oxygen isotope data from ice core NGRIP ...
title_short 50 year means of oxygen isotope data from ice core NGRIP ...
title_full 50 year means of oxygen isotope data from ice core NGRIP ...
title_fullStr 50 year means of oxygen isotope data from ice core NGRIP ...
title_full_unstemmed 50 year means of oxygen isotope data from ice core NGRIP ...
title_sort 50 year means of oxygen isotope data from ice core ngrip ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.586886
https://doi.pangaea.de/10.1594/PANGAEA.586886
genre Greenland
Greenland ice core
Greenland Ice core Project
ice core
NGRIP
North Greenland
North Greenland Ice Core Project
genre_facet Greenland
Greenland ice core
Greenland Ice core Project
ice core
NGRIP
North Greenland
North Greenland Ice Core Project
op_relation https://dx.doi.org/10.1038/nature02805
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.58688610.1038/nature02805
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