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North Atlantic climatic oscillations revealed by deep Greenland ice cores

Dansgaard, W., Johnsen, S.J., Clausen, H.B., Dahl-Jensen, D., Gundestrup, N., Hammer, C.U., Oeschger, H.·1984·Geophysical Monograph Series

Abstract

Five long-term oxygen isotope (δ) records along ice cores are discussed, in particular two from the Greenland ice sheet that exhibit persistent δ oscillations with a quasi-periodicity of ca. 2550 years. A detailed study of the δ cycles in the Wisconsin glaciation show that they cannot be ascribed to discontinuities in the cores, nor to ice-dynamic instabilities in the ice sheet. In the Holocene, the δ cycles are less pronounced, but they are concurrent with the fluctuating glacier extention elsewhere, which substantiates their climatic significance. An anti-correlation with 14C concentration in atmospheric CO2, and with 10Be deposition rates on the ice sheets, suggests a connection between climate and solar processes, but a conclusion on this point must await clarification of the terrestrial circulation and mixing processes, and the relationship between the solar outputs of radiation and particulate matter.

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Metadata

Authors
Dansgaard, W., Johnsen, S. J., Clausen, H. B., Dahl-Jensen, D., Gundestrup, N., Hammer, C. U., & Oeschger, H.
Venue
Geophysical Monograph Series
Published
1984
Pages
288-298
ISSN
0065-8448 (ISSN-L)
OpenAlex
W1491826018
Cited by
394
References
0
FWCI
12.22
Type
book chapter
Language
en
Open access
closed

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CoChat. (2026). Citation check: North Atlantic climatic oscillations revealed by deep Greenland ice cores. https://app.cochat.ai/papers/10.1029/gm029p0288
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Dansgaard, W., Johnsen, S. J., Clausen, H. B., Dahl-Jensen, D., Gundestrup, N., Hammer, C. U., & Oeschger, H. (1984). North Atlantic climatic oscillations revealed by deep Greenland ice cores. Geophysical Monograph Series. https://doi.org/10.1029/gm029p0288

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