The DOI matches its Crossref record; 3 of the 3 references it cites were found in a registry or an index.
THE DEGLACIATION OF THE NORTHERN HEMISPHERE: A Global Perspective
Abstract
▪ Abstract Orbitally induced increase in northern summer insolation after growth of a large ice sheet triggered deglaciation and associated global warming. Ice-albedo, sea-level, and greenhouse-gas feedbacks, together with tropical warming from weakening winds in response to polar amplification of warming, caused regional-to-global (near-) synchronization of deglaciation. Effects were larger at orbital rather than millennial frequencies because ice sheets and carbon dioxide vary slowly. Ice-sheet–linked changes in freshwater delivery to the North Atlantic, and possibly free oscillations in the climate system, forced millennial climate oscillations associated with changes in North Atlantic deep water (NADW) flow. The North Atlantic typically operates in one of three modes: modern, glacial, and Heinrich. Deglaciation occurred from a glacial-mode ocean that, in comparison to modern, had shallower depth of penetration of NADW formed further south, causing strong northern cooling and the widespread cold, dry, and windy conditions associated with the glacial maximum and the cold phases of the millennial Dansgaard-Oeschger oscillations. The glacial mode was punctuated by meltwater-forced Heinrich conditions that caused only small additional cooling at high northern latitudes, but greatly reduced the formation of NADW and triggered an oceanic “seesaw” that warmed some high-latitude southern regions centered in the South Atlantic.
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Citations
Cites
Asynchrony of Antarctic and Greenland climate change during the last glacial period
Blunier, T., Chappellaz, J., Schwander, J., Dällenbach, A., Stauffer, B., Stocker, T. F., Raynaud, D., Jouzel, J., Clausen, H. B., Hammer, C. U., et al. (1998) · Nature · doi:10.1038/29447 · Cited by 772
Sarnthein, M., Winn, K., Jung, S. J. A., Duplessy, J., Labeyrie, L., Erlenkeuser, H., & Ganssen, G. (1994) · Paleoceanography · doi:10.1029/93pa03301 · Cited by 652
The North Atlantic atmosphere-sea surface 14C gradient during the Younger Dryas climatic event
Bard, E., Arnold, M., Mangerud, J., Paterne, M., Labeyrie, L., Duprat, J., Mélières, M.-A., Sønstegaard, E., & Duplessy, J.-C. (1994) · Earth and Planetary Science Letters · doi:10.1016/0012-821x(94)90112-0 · Cited by 382
Cited by
The 8k event: cause and consequences of a major Holocene abrupt climate change
ALLEY, R., & AGUSTSDOTTIR, A. (2005) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2004.12.004 · Cited by 916
Self-citationIce sheet sources of sea level rise and freshwater discharge during the last deglaciation
Carlson, A. E., & Clark, P. U. (2012) · Reviews of Geophysics · doi:10.1029/2011rg000371 · Cited by 249
Self-citationPhase relationships between Antarctic and Greenland climate records
Steig, E. J., & Alley, R. B. (2002) · Annals of Glaciology · doi:10.3189/172756402781817211 · Cited by 80
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Metadata
- Authors
- Alley, R. B., & Clark, P. U.
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 1999-05
- Volume
- 27
- Issue
- 1
- Pages
- 149-182
- ISSN
- 0084-6597 (ISSN-L)
- 1545-4495
- OpenAlex
- W2136239559
- Cited by
- 328
- References
- 3
- FWCI
- 5.20
- Type
- journal article
- Language
- en
- Open access
- closed
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- Alley, R. B., & Clark, P. U. (1999). THE DEGLACIATION OF THE NORTHERN HEMISPHERE: A Global Perspective. Annual Review of Earth and Planetary Sciences. https://doi.org/10.1146/annurev.earth.27.1.149
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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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