Enhanced Atmospheric Circulation over North America During the Early Holocene: Evidence from Lake Superior
JOHN D. HALFMAN 1 and
THOMAS C. JOHNSON 1
1 Duke University Marine Laboratory, Beaufort, North Carolina 28516
Profiles of grain sizes in five cores recovered from Lake Superior show that grain size increased with burial depth to the postglacial-glacial contact. The results reflect a substantial reduction in bottom-current velocity and the corresponding wind velocity from 9500 to 6500 years ago.
Submitted on September 1, 1983
Accepted on January 10, 1984