Synchronization of ice core records via atmospheric gases

被引：49

作者：

Blunier, T. ^{[1
]}

Spahni, R. ^{[1
]}

Barnola, J. -M. ^{[2
]}

Chappellaz, J. ^{[2
]}

Loulergue, L. ^{[2
]}

Schwander, J. ^{[1
]}

机构：

[1] Univ Bern, Inst Phys, CH-3012 Bern, Switzerland

[2] CNRS UJF, LGGE, F-38402 St Martin Dheres, France

来源：

CLIMATE OF THE PAST | 2007年 / 3卷 / 02期

关键词：

D O I：

10.5194/cp-3-325-2007

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with different types of climate archives. Even for ice cores a direct synchronization between ice cores from Greenland and Antarctica has not been possible so far due to the lack of time markers occurring in both hemispheres. Fortunately, variations in the time series of global gas records can be used as indirect time markers. Here we discuss in detail the steps that are necessary to synchronize ice cores via global gas records exemplified on the synchronization of the EPICA ice core from Dronning Maud Land to a Greenland record from North GRIP.

引用

页码：325 / 330

页数：6

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