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.
Original language | English (US) |
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Pages (from-to) | 119-131 |
Number of pages | 13 |
Journal | Polar Geography |
Volume | 23 |
Issue number | 2 |
DOIs | |
State | Published - Apr 1 1999 |
All Science Journal Classification (ASJC) codes
- Geography, Planning and Development
- General Agricultural and Biological Sciences
- General Earth and Planetary Sciences