Imperial College London
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ProfessorMartinSiegert

Faculty of Natural Sciences, The Grantham Institute for Climate Change

Visiting Professor
 
 
 
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Contact

 

+44 (0)20 7594 9666m.siegert Website

 
 
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Assistant

 

Ms Gosia Gayer +44 (0)20 7594 9666

 
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Location

 

Grantham Directors OfficeSherfield BuildingSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@article{Parrenin:2017:10.5194/tc-11-2427-2017,
author = {Parrenin, F and Cavitte, MGP and Blankenship, DD and Chappellaz, J and Fischer, H and Gagliardini, O and Masson-Delmotte, V and Passalacqua, O and Ritz, C and Siegert, MJ and Roberts, J and Young, DA},
doi = {10.5194/tc-11-2427-2017},
journal = {The Cryosphere},
pages = {2427--2437},
title = {Is there 1.5 million-year old ice near Dome C, Antarctica?},
url = {http://dx.doi.org/10.5194/tc-11-2427-2017},
volume = {11},
year = {2017}
}
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RIS format (EndNote, RefMan)

TY  - JOUR
AB  - 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 ∼ 800000 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 (> 1.5Myr, 1.5 million years) likely exists in two regions: one ∼ 40km 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 10–30km 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.
AU  - Parrenin,F
AU  - Cavitte,MGP
AU  - Blankenship,DD
AU  - Chappellaz,J
AU  - Fischer,H
AU  - Gagliardini,O
AU  - Masson-Delmotte,V
AU  - Passalacqua,O
AU  - Ritz,C
AU  - Siegert,MJ
AU  - Roberts,J
AU  - Young,DA
DO  - 10.5194/tc-11-2427-2017
EP  - 2437
PY  - 2017///
SN  - 1994-0416
SP  - 2427
TI  - Is there 1.5 million-year old ice near Dome C, Antarctica?
T2  - The Cryosphere
UR  - http://dx.doi.org/10.5194/tc-11-2427-2017
UR  - http://hdl.handle.net/10044/1/53057
VL  - 11
ER  -
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