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Complexity of Holocene Climate as Reconstructed from a Greenland Ice Core

O'Brien, S. R., Mayewski, P. A., Meeker, L. D., Meese, D. A., Twickler, M. S., Whitlow, S. I.·1995·Science

Abstract

Glaciochemical time series developed from Summit, Greenland, indicate that the chemical composition of the atmosphere was dynamic during the Holocene epoch. Concentrations of sea salt and terrestrial dusts increased in Summit snow during the periods 0 to 600, 2400 to 3100, 5000 to 6100, 7800 to 8800, and more than 11,300 years ago. The most recent increase, and also the most abrupt, coincides with the Little Ice Age. These changes imply that either the north polar vortex expanded or the meridional air flow intensified during these periods, and that temperatures in the mid to high northern latitudes were potentially the coldest since the Younger Dryas event.

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Metadata

Authors
O'Brien, S. R., Mayewski, P. A., Meeker, L. D., Meese, D. A., Twickler, M. S., & Whitlow, S. I.
Venue
Science
Published
1995-12-22
Volume
270
Issue
5244
Pages
1962-1964
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1964366413
Cited by
912
References
0
FWCI
14.51
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Complexity of Holocene Climate as Reconstructed from a Greenland Ice Core. https://app.cochat.ai/papers/10.1126/science.270.5244.1962
The paper
O'Brien, S. R., Mayewski, P. A., Meeker, L. D., Meese, D. A., Twickler, M. S., & Whitlow, S. I. (1995). Complexity of Holocene Climate as Reconstructed from a Greenland Ice Core. Science. https://doi.org/10.1126/science.270.5244.1962

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.