Early-warning signals for Dansgaard-Oeschger events in a high-resolution ice core record

The Dansgaard-Oeschger (DO) events, as observed in oxygen isotope ratios from the North Greenland Ice Core Project (NGRIP) record, are an outstanding example of past abrupt climate transitions. Their physical cause remains debated, and previous research indicated that they are not preceded by classi...

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Main Author: Boers, N.
Format: Article in Journal/Newspaper
Language:English
Published: London : Nature Publishing Group 2018
Subjects:
Online Access:https://oa.tib.eu/renate/handle/123456789/5139
https://doi.org/10.34657/3768
id fttibhannoverren:oai:oa.tib.eu:123456789/5139
record_format openpolar
spelling fttibhannoverren:oai:oa.tib.eu:123456789/5139 2024-09-09T19:37:46+00:00 Early-warning signals for Dansgaard-Oeschger events in a high-resolution ice core record Boers, N. 2018 application/pdf https://oa.tib.eu/renate/handle/123456789/5139 https://doi.org/10.34657/3768 eng eng London : Nature Publishing Group DOI:https://doi.org/10.1038/s41467-018-04881-7 https://oa.tib.eu/renate/handle/123456789/5139 https://doi.org/10.34657/3768 CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ frei zugänglich ddc:550 Dansgaard–Oeschger (DO) events North Greenland Ice Core Project (NGRIP) climate change status-type:publishedVersion doc-type:Article doc-type:Text 2018 fttibhannoverren https://doi.org/10.34657/376810.1038/s41467-018-04881-7 2024-07-03T23:33:53Z The Dansgaard-Oeschger (DO) events, as observed in oxygen isotope ratios from the North Greenland Ice Core Project (NGRIP) record, are an outstanding example of past abrupt climate transitions. Their physical cause remains debated, and previous research indicated that they are not preceded by classical early-warning signals (EWS). Subsequent research hypothesized that the DO events are caused by bifurcations of physical mechanisms operating at decadal timescales, and proposed to search for EWS in the high-frequency fluctuation levels. Here, a time series with 5-year resolution is obtained from the raw NGRIP record, and significant numbers of EWS in terms of variance and autocorrelation increases are revealed in the decadal-scale variability. Wavelet analysis indicates that the EWS are most pronounced in the 10-50-year periodicity band, confirming the above hypothesis. The DO events are hence neither directly noise-induced nor purely externally forced, which provides valuable constraints regarding potential physical causes. Article in Journal/Newspaper Dansgaard-Oeschger events Greenland Greenland ice core Greenland Ice core Project ice core NGRIP North Greenland North Greenland Ice Core Project Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover) Greenland
institution Open Polar
collection Renate - Repositorium für Naturwissenschaften und Technik (TIB Hannover)
op_collection_id fttibhannoverren
language English
topic ddc:550
Dansgaard–Oeschger (DO) events
North Greenland Ice Core Project (NGRIP)
climate change
spellingShingle ddc:550
Dansgaard–Oeschger (DO) events
North Greenland Ice Core Project (NGRIP)
climate change
Boers, N.
Early-warning signals for Dansgaard-Oeschger events in a high-resolution ice core record
topic_facet ddc:550
Dansgaard–Oeschger (DO) events
North Greenland Ice Core Project (NGRIP)
climate change
description The Dansgaard-Oeschger (DO) events, as observed in oxygen isotope ratios from the North Greenland Ice Core Project (NGRIP) record, are an outstanding example of past abrupt climate transitions. Their physical cause remains debated, and previous research indicated that they are not preceded by classical early-warning signals (EWS). Subsequent research hypothesized that the DO events are caused by bifurcations of physical mechanisms operating at decadal timescales, and proposed to search for EWS in the high-frequency fluctuation levels. Here, a time series with 5-year resolution is obtained from the raw NGRIP record, and significant numbers of EWS in terms of variance and autocorrelation increases are revealed in the decadal-scale variability. Wavelet analysis indicates that the EWS are most pronounced in the 10-50-year periodicity band, confirming the above hypothesis. The DO events are hence neither directly noise-induced nor purely externally forced, which provides valuable constraints regarding potential physical causes.
format Article in Journal/Newspaper
author Boers, N.
author_facet Boers, N.
author_sort Boers, N.
title Early-warning signals for Dansgaard-Oeschger events in a high-resolution ice core record
title_short Early-warning signals for Dansgaard-Oeschger events in a high-resolution ice core record
title_full Early-warning signals for Dansgaard-Oeschger events in a high-resolution ice core record
title_fullStr Early-warning signals for Dansgaard-Oeschger events in a high-resolution ice core record
title_full_unstemmed Early-warning signals for Dansgaard-Oeschger events in a high-resolution ice core record
title_sort early-warning signals for dansgaard-oeschger events in a high-resolution ice core record
publisher London : Nature Publishing Group
publishDate 2018
url https://oa.tib.eu/renate/handle/123456789/5139
https://doi.org/10.34657/3768
geographic Greenland
geographic_facet Greenland
genre Dansgaard-Oeschger events
Greenland
Greenland ice core
Greenland Ice core Project
ice core
NGRIP
North Greenland
North Greenland Ice Core Project
genre_facet Dansgaard-Oeschger events
Greenland
Greenland ice core
Greenland Ice core Project
ice core
NGRIP
North Greenland
North Greenland Ice Core Project
op_relation DOI:https://doi.org/10.1038/s41467-018-04881-7
https://oa.tib.eu/renate/handle/123456789/5139
https://doi.org/10.34657/3768
op_rights CC BY 4.0 Unported
https://creativecommons.org/licenses/by/4.0/
frei zugänglich
op_doi https://doi.org/10.34657/376810.1038/s41467-018-04881-7
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