Surface characteristics at Dome A, Antarctica: first measurements and a guide to future ice-coring sites

An assessment of the glaciological and meteorological characteristics of Dome A, the summit of the East Antarctic ice sheet, is made based on field investigations during the austral summer of 2004/05. Knowledge of these characteristics is critical for future international studies such as deep ice-co...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Cunde, Xiao, Yuansheng, Li, Allison, Ian, Shugui, Hou, Dreyfus, Gabrielle, Barnola, Jean-Marc, Jiawen, Ren, Lingen, Bian, Shenkai, Zhang, Kameda, Takao
Language:English
Published: International Glaciological Society 2008
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Online Access:https://kitami-it.repo.nii.ac.jp/record/8059/files/2008_Surface characteristics at Dome A, Antarctica first measurements and a guide to future ice-coring sites.pdf
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Summary:An assessment of the glaciological and meteorological characteristics of Dome A, the summit of the East Antarctic ice sheet, is made based on field investigations during the austral summer of 2004/05. Knowledge of these characteristics is critical for future international studies such as deep ice-core drilling. The assessment shows that: (1) Dome A is characterized by a very low 10 m depth firn temperature, ?58.3°C (nearly 3°C lower than at EPICA Dome C and 1°C lower than at Vostok). (2) Automatic weather station (AWS) measurements of snow surface height and reference layers in a snow pit indicate the present-day snow accumulation rate at Dome A is within the range 1?3 cm w.e.a?1. Densification models suggest a range of 1?2 cm w.e.a?1. This is lower than at other sites along the ice divide of East Antarctica (IDEA). Annual layers at Dome A are thus potentially thinner than at other sites, so that a longer record is preserved in a given ice thickness. (3) The average wind speed observed at Dome A (<4 m s?1) is lower than at other sites along IDEA. Together, these parameters, combined with radio-echo sounding data and information on the subglacial drainage distribution beneath Dome A, suggest Dome A as a candidate site for obtaining the oldest ice core. journal article