Evidence for solar forcing of climate variation from δ18O of peat cellulose

被引:25
|
作者
Hong, YT [1 ]
Liu, DS
Jiang, HB
Zhou, LP
Beer, J
Hong, B
Zhu, YX
Li, HD
Leng, XT
Qin, XG
Wang, Y
Lin, QH
Zeng, YQ
机构
[1] Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, Guiyang 550002, Peoples R China
[2] Chinese Acad Sci, Inst Geol, Beijing 100029, Peoples R China
[3] Univ Cambridge, Dept Earth Sci, Godwin Lab, Cambridge CB2 3SA, England
[4] EAWAG, CH-8600 Dubendorf, Switzerland
[5] NE Normal Univ, Inst Peatmire, Changchun 130024, Peoples R China
来源
关键词
solar variability; climatic change; peat; delta O-18; radiocarbon anomalies;
D O I
10.1007/BF02878152
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
There have been a number of investigations for examining the possible link between long-term climate variability and solar activity, A continuous delta(18)O record of peat cellulose covering the past 6 000 years and the response of climate variation inferred from the proxy record to solar forcing are reported. Results show that during the past 5 000 years the abrupt climate variations, including 17 warming and 17 cooling, and a serious of periodicities, such as 86, 101, 110, 127, 132, 140, 155, 207, 245, 311, 820 and 1 050 years, are strikingly correlative to the changes of solar irradiation and periodicity. These observations are considered as further evidence for a close relationship between solar activity and climate variations on time scales of decades to centuries.
引用
收藏
页码:217 / 224
页数:8
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