An improved North-South synchronization of ice core records around the 41 K beryllium 10 peak

Using new high-resolution 10Be measurements in the NGRIP, EDML and Vostok ice cores, together with previously published data from EDC, we present an improved synchronization between Greenland and Antarctic ice cores during the Laschamp geomagnetic excursion ∼ 41 kyr ago. We estimate the precision of this synchronization to be ±20 years, an order of magnitude better than previous work. We discuss the implications of this new synchronization for making improved estimates of the depth difference between ice and enclosed gas of the same age (1depth), difference between age of ice and enclosed gas at the same depth (1age) in the EDC and EDML ice cores, spectral properties of the 10Be profiles and phasing between Dansgaard–Oeschger-10 (in NGRIP) and AIM-10 (in EDML and EDC).

• Publication year

  2016

• Venue

  Climate of The Past Discussions

• Publication date

  2016-07-28

• Fields of study

  Geology, Physics, Environmental Science

• Identifiers
  DOI 10.5194/CP-2016-79
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

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