File:Figure 3.13 - Methane and d18O records covering the period 10-60 ka ago.png
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Figure_3.13_-_Methane_and_d18O_records_covering_the_period_10-60_ka_ago.png (534 × 507 pixels, file size: 185 KB, MIME type: image/png)
Methane (CH4) synchronization of the ice core records of δ18O as a proxy for temperature reveals one-to-one association of Antarctic warming (AIM) events with corresponding Greenland cold (stadial) events (D/O) covering the period 10-60 ka ago. EDML = EPICA core from Dronning Maud Land Antarctica, Byrd = core from West Antarctica; EDC = core from East Antarctica; NGRIP = core from North Greenland. Gray bars refer to Greenland stadial periods. Figure modified from EPICA (2006[1]) by H. Fischer (from Mayewski et al., 2009[2]).
- ↑ EPICA community members. 2006. One-to-one coupling of glacial climate variability in Greenland and Antarctica, Nature, 444, 195-198.
- ↑ Mayewski, P.A., Meredith, M.P., Summerhayes, C.P., Turner, J., Worby, A.P., Barrett, P.J., Casassa, G., Bertler, N.A.N., Bracegirdle, T.J., Naveira-Garabato, A.C., Bromwich, D.H., Campbell, H., Hamilton, G.H., Lyons, W.B., Maasch, K.A., Aoki, S., and Xiao, C. 2009. State of the Antarctic and Southern Ocean Climate System (SASOCS), Reviews of Geophysics, 47, RG1003, doi:10.1029/2007RG000231.
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