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Cited by 521

The DOI matches its Crossref record; 49 of the 49 references it cites were found in a registry or an index.

North Atlantic ocean circulation and abrupt climate change during the last glaciation

Open access
Henry, L. G., McManus, J. F., Curry, W. B., Roberts, N. L., Piotrowski, A. M., Keigwin, L. D.·2016·Science

Abstract

An ocean of climate impacts: Large decreases in Atlantic meridional overturning circulation accompanied every one of the cold Northern Hemispheric stadial events that occurred during the heart of the last glacial period. These events, lasting on average around 1000 years each, have long been thought to result from changes in deep ocean circulation. Henry et al. used a suite of geochemical proxies from marine sediments to show that reductions in the export of northern deep waters occurred before and during stadial periods (see the Perspective by Schmittner). This observation firmly establishes the role of ocean circulation as a cause of abrupt glacial climate change during that interval. Science , this issue p. 470 ; see also p. 445

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Metadata

Authors
Henry, L. G., McManus, J. F., Curry, W. B., Roberts, N. L., Piotrowski, A. M., & Keigwin, L. D.
Venue
Science
Published
2016-07-29
Volume
353
Issue
6298
Pages
470-474
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2460928081
Cited by
521
References
49
FWCI
20.53
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: North Atlantic ocean circulation and abrupt climate change during the last glaciation. https://app.cochat.ai/papers/10.1126/science.aaf5529
The paper
Henry, L. G., McManus, J. F., Curry, W. B., Roberts, N. L., Piotrowski, A. M., & Keigwin, L. D. (2016). North Atlantic ocean circulation and abrupt climate change during the last glaciation. Science. https://doi.org/10.1126/science.aaf5529

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

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