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High mid-Holocene accumulation rates over West Antarctica inferred from a pervasive ice-penetrating radar reflector
by
J. A. Bodart
,
R. G. Bingham
,
D. A. Young
,
J. A. MacGregor
,
D. W. Ashmore
,
E. Quartini
,
A. S. Hein
,
D. G. Vaughan
,
D. D. Blankenship
Published in
The Cryosphere
(2023)
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GE1-350
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Pine Island Glacier
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