Spatial and temporal distributions of surface mass balance between Concordia and Vostok stations, Antarctica, from combined radar and ice core data: first results and detailed error analysis

Results from ground-penetrating radar (GPR) measurements and shallow ice cores carried out during a scientific traverse between Dome Concordia (DC) and Vostok stations are presented in order to infer both spatial and temporal characteristics of snow accumulation over the East Antarctic Plateau....

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Bibliographic Details
Main Authors: E. Le Meur, O. Magand, L. Arnaud, M. Fily, M. Frezzotti, M. Cavitte, R. Mulvaney, S. Urbini
Format: Article
Language:English
Published: Copernicus Publications 2018-05-01
Series:The Cryosphere
Online Access:https://www.the-cryosphere.net/12/1831/2018/tc-12-1831-2018.pdf