Phase relationships between orbital forcing and the composition of air trapped in Antarctic ice cores
Orbital tuning is central for ice core chronologies beyond annual layer counting, available back to 60 ka (i.e. thousands of years before 1950) for Greenland ice cores. While several complementary orbital tuning tools have recently been developed using δ 18 O atm , δ O 2 ⁄N 2 and air content with di...
Published in: | Climate of the Past |
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Main Authors: | , , , , , , , , , |
Format: | Text |
Language: | English |
Published: |
2018
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Subjects: | |
Online Access: | https://doi.org/10.5194/cp-12-729-2016 https://cp.copernicus.org/articles/12/729/2016/ |