Abstract
Samples of surface snow were collected for stable isotope analysis along the traverse route from Zhongshan to Dome A (East Antarctica) from Dec 28th, 2007 to Feb. 8th, 2008. The local relationship between δD and surface temperature is established to be 6.4 ± 0.2 ‰ per °C, very similar to the average for East Antarctic. The deuterium excess shows a pattern of high values over Antarctica, particularly at Dome A. We compare our data with an atmospheric general circulation model which includes stable water isotopes (ECHAM5-wiso). The model simulation captures the right levels of δD, but overestimates δ18O. This study provides support for the ongoing deep ice core project at Dome A.
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Acknowledgments
We are thankful for logistical support provided by CHINARE. This study was funded by the National Natural Science Foundation of China (41206179; 41121001), the State Oceanic Administration of People’s Republic of China Project on Climate in Polar Regions (CHINARE2012-02-02,CHINARE2012-04-04) and Post-Doctor Fund (2011M500462). LSCE support from ANR VANISH and Dome A is acknowledged. Ian Allison helped both in science and English.
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Xiao, C., Ding, M., Masson-Delmotte, V. et al. Stable isotopes in surface snow along a traverse route from Zhongshan station to Dome A, East Antarctica. Clim Dyn 41, 2427–2438 (2013). https://doi.org/10.1007/s00382-012-1580-0
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DOI: https://doi.org/10.1007/s00382-012-1580-0