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Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth

Ruddiman, W. F., McIntyre, A.·1979·Science

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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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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CoChat. (2026). Citation check: Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth. https://app.cochat.ai/papers/10.1126/science.204.4389.173
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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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