Journal
HOLOCENE
Volume 14, Issue 2, Pages 145-151Publisher
SAGE PUBLICATIONS LTD
DOI: 10.1191/0959683604hl697ft
Keywords
millennial-scale variability; climatic variations; ice core; EPICA; Southern Ocean; Dome C; isotopic modelling; Climatic Optimum; Holocene; Antarctica
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Measurements of the two water stable isotopes (deltaD and delta(18)O) along EPICA (European Project for Ice Coring in Antarctica) Dome C ice core are combined with simple isotopic modelling (distillation models) to construct the variability of both the site temperature (East Antarctica) and the moisture source temperature (nowadays probably the subantarctic Indian Ocean). We discuss the difference between the reconstructed site and source temperature profiles with respect to the initial isotopic data. We show that (i) the early-Holocene optimum appears first in Antarctica and 800 years later in the Southern Ocean, and (ii) during the last 5000 years, the site and source temperatures co-vary at the centennial timescale. An 833-year periodicity is observed only on deuterium and site temperature and therefore probably of local origin.
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