Climate and Dynamics
Atmospheric methane during the last four glacial-interglacial cycles: Rapid changes and their link with Antarctic temperature
Article first published online: 24 JUN 2004
Copyright 2004 by the American Geophysical Union.
Journal of Geophysical Research: Atmospheres (1984–2012)
Volume 109, Issue D12, 27 June 2004
How to Cite
2004), Atmospheric methane during the last four glacial-interglacial cycles: Rapid changes and their link with Antarctic temperature, J. Geophys. Res., 109, D12104, doi:10.1029/2003JD004417., , , , , , , and (
- Issue published online: 24 JUN 2004
- Article first published online: 24 JUN 2004
- Manuscript Accepted: 30 MAR 2004
- Manuscript Revised: 6 MAR 2004
- Manuscript Received: 4 DEC 2003
- atmospheric methane;
- ice core
 Atmospheric methane (CH4) recorded in Antarctic ice cores represents the closest ice proxy available for Greenland temperature changes beyond times when Greenland climate records are available. The record over four climatic cycles from the Vostok ice core offers the opportunity to study the phase relationship between Greenland and Antarctic climate changes through detailed CH4 profiles. Combining American and French analytical efforts, we have improved the time resolution of the existing CH4 record from Petit et al. . Spectral analyses reveal high- and low-frequency variability (including a strong precessional component). The phase relationship between CH4 and the Antarctic temperature proxy (δD) shows a systematic lag of CH4 versus temperature by 1100 ± 200 years, on long timescales (50–400 kyr) and a more complex behavior over shorter timescales (i.e., ≤25 kyr), suggesting that Dansgaard/Oeschger-type of climatic variability and associated interhemispheric linkage are robust features of late Quaternary climate.