Abstract
Ice-core records show that climate changes in the past have been large, rapid, and synchronous over broad areas extending into low latitudes, with less variability over historical times. These ice-core records come from high mountain glaciers and the polar regions, including small ice caps and the large ice sheets of Greenland and Antarctica.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 1331-1334 |
| Number of pages | 4 |
| Journal | Proceedings of the National Academy of Sciences of the United States of America |
| Volume | 97 |
| Issue number | 4 |
| DOIs | |
| State | Published - Feb 15 2000 |
All Science Journal Classification (ASJC) codes
- General
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