Articles | Volume 20, issue 7
https://doi.org/10.5194/tc-20-3977-2026
https://doi.org/10.5194/tc-20-3977-2026
Research article
 | 
20 Jul 2026
Research article |  | 20 Jul 2026

Late Holocene stabilization of Conway Ice Ridge

Andrew O. Hoffman, Paul T. Summers, Jenny Suckale, Knut Christianson, Ginny Catania, and Howard Conway

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Cited articles

Alley, K. E., Scambos, T. A., Anderson, R. S., Rajaram, H., Pope, A., and Haran, T. M.: Continent-wide estimates of Antarctic strain rates from Landsat 8-derived velocity grids, J. Glaciol., 64, 321–332, https://doi.org/10.1017/jog.2018.23, 2018. a
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Bindschadler, R.: Siple Coast Project research of Crary Ice Rise and the mouths of Ice Streams B and C, West Antarctica: review and new perspectives, J. Glaciol., 39, 538–552, https://doi.org/10.3189/S0022143000016439, 1993. a
Bindschadler, R., Vornberger, P., Blankenship, D., Scambos, T., and Jacobel, R.: Surface velocity and mass balance of Ice Streams D and E, West Antarctica, J. Glaciol., 42, 461–475, https://doi.org/10.3189/s0022143000003452, 1996. a
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Short summary
In Antarctica, fast-flowing ice streams drive most ice loss. Radar data from Conway Ice Ridge reveal that the van der Veen and Mercer Ice Streams were wider ~3000 years ago and narrowed progressively. Numerical modeling demonstrates that small thickness changes can rapidly alter shear-margin locations. These findings offer crucial insights into Late Holocene Ice Sheet readvance.
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