Antarctic firn compaction rates from repeat-track airborne radar data: I. Methods

While measurements of ice-sheet surface elevation change are increasingly used to assess mass change, the processes that control the elevation fluctuations not related to ice-flow dynamics (e.g. firn compaction and accumulation) remain difficult to measure. Here we use radar data from the Thwaites G...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Medley, B., Ligtenberg, S. R. M., Joughin, Ian R., van den Broeke, Michiel R., Gogineni, Sivaprasad, Nowicki, S.
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 2016
Subjects:
Online Access:http://hdl.handle.net/1808/22196
https://doi.org/10.3189/2015AoG70A203