Statistics of the recurrence rate analysis for U1308 benthic δ18O, U1308 bulk carbonate δ18O and NGRIP δ18O

Statistics of the recurrence rate analysis for U1308 benthic δ18O, U1308 bulk carbonate δ18O (Hodell and Channell, 2016) and NGRIP δ18O (Rasmussen et al., 2014). The RR prominence higher than RR standard deviation are considered as major transitions and labeled with a red cross on Figs. 2a, 3a and 4...

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Bibliographic Details
Main Authors: Rousseau, Denis-Didier, Bagniewski, Witold, Ghil, Michael
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
303-U1308
abrupt climate changes
AGE
astronomical theory of climate
Bond cycles
COMPCORE
Composite Core
Dansgaard-Oeschger events
Event label
Exp303
Greenland
Heinrich events
ICEDRILL
Ice drill
Ice Rafted Debris
ice sheets
Interval
Joides Resolution
Material
NGRIP
North Atlantic
North Atlantic Climate 1
NorthGRIP
Recurrence rate prominence
Sampling/drilling ice
Significance
description
TiPES
Tipping Points in the Earth System
Rasmussen
Rousseau
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.942620
https://doi.org/10.1594/PANGAEA.942620
Description
Summary:Statistics of the recurrence rate analysis for U1308 benthic δ18O, U1308 bulk carbonate δ18O (Hodell and Channell, 2016) and NGRIP δ18O (Rasmussen et al., 2014). The RR prominence higher than RR standard deviation are considered as major transitions and labeled with a red cross on Figs. 2a, 3a and 4c (Rousseau, Denis-Didier; et al., 2022). RR prominence slightly lower to the standard variation are identified with an asterisk and labeled with pink cross on the same figures. RR prominence significance: # above the standard deviation (sd), $ slightly lower than the standard deviation. The window size of the statistical analysis is also given for every record in column 2.

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