Author:
Reeh N.,Clausen H.B.,Dansgaard W.,Gundestrup N.,Hammer C.U.,Johnsen S.J.
Abstract
AbstractThe annual layer thickness profiles along three 400 m ice cores are transferred into accumulation-rate records. A linear decrease of 3±2% per millenium is found in mid-Greenland. Intermediate-term (periods longer than 120 years) deviations from the linear trend lines are less than 5% in mid-Greenland but reach 11% at Dye 3 around A.D. 1700 and 1400. Short-term (periods between 120 and 30 years) oscillations are generally in phase at Milcent and Crête.
Publisher
Cambridge University Press (CUP)
Cited by
50 articles.
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