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Iceberg Discharges into the North Atlantic on Millennial Time Scales During the Last Glaciation
Abstract
High-resolution studies of North Atlantic deep sea cores demonstrate that prominent increases in iceberg calving recurred at intervals of 2000 to 3000 years, much more frequently than the 7000- to 10,000-year pacing of massive ice discharges associated with Heinrich events. The calving cycles correlate with warm-cold oscillations, called Dansgaard-Oeschger events, in Greenland ice cores. Each cycle records synchronous discharges of ice from different sources, and the cycles are decoupled from sea-surface temperatures. These findings point to a mechanism operating within the atmosphere that caused rapid oscillations in air temperatures above Greenland and in calving from more than one ice sheet.
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Metadata
- Authors
- Bond, G. C., & Lotti, R.
- Venue
- Science
- Published
- 1995-02-17
- Volume
- 267
- Issue
- 5200
- Pages
- 1005-1010
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W2051559013
- Cited by
- 1,290
- References
- 0
- FWCI
- 49.70
- Type
- journal article
- Language
- en
- Open access
- closed
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