globalchange  > 影响、适应和脆弱性
DOI: 10.5194/tc-11-2427-2017
Scopus记录号: 2-s2.0-85027444602
论文题名:
Is there 1.5-million-year-old ice near Dome C, Antarctica?
作者: Parrenin F; , Cavitte M; G; P; , Blankenship D; D; , Chappellaz J; , Fischer H; , Gagliardini O; , Masson-Delmotte V; , Passalacqua O; , Ritz C; , Roberts J; , Siegert M; J; , Young D; A
刊名: Cryosphere
ISSN: 19940416
出版年: 2017
卷: 11, 期:6
起始页码: 2427
结束页码: 2437
语种: 英语
英文关键词: age determination ; basal ice ; flow modeling ; ice core ; ice flow ; ice sheet ; paleoclimate ; proxy climate record ; radar ; Antarctica ; Dome Concordia ; East Antarctica
英文摘要: Ice sheets provide exceptional archives of past changes in polar climate, regional environment and global atmospheric composition. The oldest dated deep ice core drilled in Antarctica has been retrieved at EPICA Dome C (EDC), reaching ∼ 800 000 years. Obtaining an older paleoclimatic record from Antarctica is one of the greatest challenges of the ice core community. Here, we use internal isochrones, identified from airborne radar coupled to ice-flow modelling to estimate the age of basal ice along transects in the Dome C area. Three glaciological properties are inferred from isochrones: surface accumulation rate, geothermal flux and the exponent of the Lliboutry velocity profile. We find that old ice (> 1.5 Myr, 1.5 million years) likely exists in two regions: one ∼ 40 km south-west of Dome C along the ice divide to Vostok, close to a secondary dome that we name "Little Dome C" (LDC), and a second region named "North Patch" (NP) located 10–30 km north-east of Dome C, in a region where the geothermal flux is apparently relatively low. Our work demonstrates the value of combining radar observations with ice flow modelling to accurately represent the true nature of ice flow, and understand the formation of ice-sheet architecture, in the centre of large ice sheets.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/75488
Appears in Collections:影响、适应和脆弱性
气候变化与战略

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作者单位: Univ. Grenoble Alpes, CNRS, IRD, IGE, Grenoble, France; Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, United States; Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, United States; Climate and Environmental Physics, Physics Institute, Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland; Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ/IPSL, UMR8212, Gif-sur-Yvette, France; Australian Antarctic Division, Kingston, TAS, Australia; Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, TAS, Australia; Grantham Institute, Department of Earth Science and Engineering, Imperial College London, London, United Kingdom

Recommended Citation:
Parrenin F,, Cavitte M,G,et al. Is there 1.5-million-year-old ice near Dome C, Antarctica?[J]. Cryosphere,2017-01-01,11(6)
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