High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector

Modelling the past and future evolution of the West Antarctic Ice Sheet (WAIS) to atmospheric and ocean forcing is challenged by the availability and quality of observed palaeo-boundary conditions. Key potential data for reconstructing past ice-sheet processes on large spatial scales are Internal Re...

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Bibliographic Details
Main Authors: Bodart, Julien A., Bingham, Robert G., Young, Duncan A., MacGregor, Joseph A., Ashmore, David W., Quartini, Enrica, Hein, Andrew S., Vaughan, David G., Blankenship, Donald D.
Format: Text
Language:English
Published: 2022
Subjects:
Antarctic
Pine Island Glacier
Ross Sea
Thwaites Glacier
Weddell
West Antarctic Ice Sheet
West Antarctica
Antarc*
Antarctica
ice core
Ice Sheet
Pine Island
Online Access:https://doi.org/10.5194/tc-2022-199
https://tc.copernicus.org/preprints/tc-2022-199/

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