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Increasing North Atlantic climate variability recorded in a central Greenland ice core
Abstract
Greenland ice-core data show that the multiannual variability in North Atlantic climate has been increasing in the latter part of the Holocene. Statistically significant trends were established before the Industrial Revolution. A general inverse correlation exists between variability and temperature, and may be linked to North Atlantic oceanic heat transport. © 1999 Taylor & Francis Group, LLC. All rights reserved.
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