Two modes of glacial climate during the late stage 5 identified in Greenland ice core records

International audience From a detailed analysis of marine and terrestrial aerosol tracers in the NGRIP ice core we identified two distinct glacial atmospheric flow patterns. The climate transition from Marine Isotope Stage 5 (MIS 5) to MIS 4, at approximately 75 kyr BP, marks a shift between two dif...

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Bibliographic Details
Main Authors: Siggaard-Andersen, M.-L., Ditlevsen, P. D., Walløe Hansen, A., Johnsen, S. J.
Other Authors: Niels Bohr Institute Copenhagen (NBI), Faculty of Science Copenhagen, University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH), Department of Bentho-pelagic processes, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Greenland
Greenland ice core
GRIP
ice core
Ice Sheet
NGRIP
North Atlantic
Online Access:https://hal.archives-ouvertes.fr/hal-00298174
https://hal.archives-ouvertes.fr/hal-00298174/document
https://hal.archives-ouvertes.fr/hal-00298174/file/cpd-3-285-2007.pdf
Description
Summary:International audience From a detailed analysis of marine and terrestrial aerosol tracers in the NGRIP ice core we identified two distinct glacial atmospheric flow patterns. The climate transition from Marine Isotope Stage 5 (MIS 5) to MIS 4, at approximately 75 kyr BP, marks a shift between two different atmospheric flow regimes. Before this transition, during MIS 5d-a, the state of atmospheric flow was alternating between the two modes of different flow patterns, while a more persistent flow pattern was prevailing through the glacial period afterwards. These changes are accompanied by strong changes in an independent Greenland ice core proxy, namely the deuterium excess from the GRIP ice core, reflecting changes in the hydrological cycle and moisture source temperatures as well. The changes in atmospheric flow pattern are correlated with changed extent of ice-rafted detritus (IRD) deposition in the North Atlantic, indicating that the state of the atmospheric flow was highly sensitive to the waxing and waning of the Laurentide ice sheet.

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