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- W2017862207 abstract "Abstract The European Project for Ice Coring in Antarctica (EPICA) focuses on the drilling of two deep ice cores, the first at Dome C and the second at Kohnen station (75°00’ S, 0°04’ E) in Dronning Maud Land (DML). This paper deals with stable-isotope records from ice cores drilled in DML. In the first season, the deep EPICA DML core reached a depth of 450 m, recovering ice approximately 7000 years old. Generally, the δ 18 O record indicates a stable Holocene climate and shows low variability. However, during the last 4000 years (based on a preliminary time-scale) the δ 18 O values decrease continuously by about 0.6%, and the deuterium excess values increase by about 0.5%. The correlation between δ 18 O and the deuterium excess d is investigated for a 50m long core section and the near-surface snow. High-pass filtered profiles are positively correlated, whereas the correlation between low-pass filtered profiles is negative. A post-depositional effect due to diffusion processes can be seen in a sub-annually resolved profile from snow-pit samples. Changes in the seasonality of the evolution of the snow cover and the consequences for stable-isotope content are demonstrated with data from ice core B31." @default.
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- W2017862207 date "2004-01-01" @default.
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- W2017862207 title "The EPICA ice core from Dronning Maud Land: first results from stable-isotope measurements" @default.
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- W2017862207 doi "https://doi.org/10.3189/172756404781814032" @default.
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