Allerod oscillation

Allerod oscillation

[′al·ə‚räd ‚äs·ə′lā·shən]
(climatology)
A temporary increase in temperature during the closing stages of the Pleistocene ice age, dated in Europe about 9850-8850 B.C.
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.