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Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth
Abstract
Two 10,000-year periods of Northern Hemisphere continental ice-sheet growth stand out prominently within the last full interglacial-to-glacial cycle. During the first half of each rapid ice-growth phase, the subpolar North Atlantic from 40°N to 60°N maintained warm sea-surface temperatures comparable to those of today's ocean. The juxtaposition at latitudes 50°N to 60°N of an "interglacial" ocean alongside a "glacial" land mass, particularly along eastern North America, is regarded as an optimal configuration for delivering moisture to the growing ice sheets.
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Cited by
Martinson, D. G., Pisias, N. G., Hays, J. D., Imbrie, J., Moore, T. C., & Shackleton, N. J. (1987) · Quaternary Research · doi:10.1016/0033-5894(87)90046-9 · Cited by 3,303
Interglacials of the last 800,000 years
Past Interglacials Working Group of PAGES (2016) · Reviews of Geophysics · doi:10.1002/2015rg000482 · Cited by 606
Dansgaard, W., Clausen, H. B., Gundestrup, N., Hammer, C. U., Johnsen, S. F., Kristinsdottir, P. M., & Reeh, N. (1982) · Science · doi:10.1126/science.218.4579.1273 · Cited by 600
Keigwin, L. (1982) · Science · doi:10.1126/science.217.4557.350 · Cited by 507
Volcanic winter and accelerated glaciation following the Toba super-eruption
Rampino, M. R., & Self, S. (1992) · Nature · doi:10.1038/359050a0 · Cited by 428
Metadata
- Authors
- Ruddiman, W. F., & McIntyre, A.
- Venue
- Science
- Published
- 1979-04-13
- Volume
- 204
- Issue
- 4389
- Pages
- 173-175
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2053568814
- Cited by
- 201
- References
- 0
- FWCI
- 17.17
- Type
- journal article
- Language
- en
- Open access
- closed
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- Ruddiman, W. F., & McIntyre, A. (1979). Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth. Science. https://doi.org/10.1126/science.204.4389.173
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