By:
Michael Bender
Princeton University
When: | Friday, April 26, 2013, 10:30 a.m. to 11:30 a.m. Join us for coffee beginning at 10:00 a.m. |
Where: | Seminar Conference Room, 10100 Burnet Road, Bldg 196-ROC, Austin, Texas 78758 |
Host: | Terry Quinn, UTIG |
Click for a Live Broadcast.
Abstract
Earth's climate oscillated between glacial and interglacial conditions with a period of 40 kyr between about 2.8 Ma and 0.9 Ma, and a period of 100 kyr since. Many important climate properties are recorded in ice cores dating to about 130 ka in Greenland and 800 ka in Antarctica. Major results will be summarized, along with efforts to extend the Greenland and Antarctic ice core records to earlier times.