Richard C A Hindmarsh
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Explore the profile of Richard C A Hindmarsh including associated specialties, affiliations and a list of published articles.
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6
Citations
78
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Recent Articles
1.
Pritchard H, Fretwell P, Fremand A, Bodart J, Kirkham J, Aitken A, et al.
Sci Data
. 2025 Mar;
12(1):414.
PMID: 40064916
We present Bedmap3, the latest suite of gridded products describing surface elevation, ice-thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60 °S. Bedmap3 incorporates and...
2.
Ritz C, Edwards T, Durand G, Payne A, Peyaud V, Hindmarsh R
Nature
. 2015 Nov;
528(7580):115-8.
PMID: 26580020
Large parts of the Antarctic ice sheet lying on bedrock below sea level may be vulnerable to marine-ice-sheet instability (MISI), a self-sustaining retreat of the grounding line triggered by oceanic...
3.
Sergienko O, Hindmarsh R
Science
. 2013 Nov;
342(6162):1086-9.
PMID: 24200815
Fast-flowing glaciers and ice streams are pathways for ice discharge from the interior of the Antarctic Ice Sheet to ice shelves, at rates controlled by conditions at the ice-bed interface....
4.
Williams C, Hindmarsh R, Arthern R
Proc Math Phys Eng Sci
. 2012 Dec;
468(2147):3285-3310.
PMID: 23197934
Changes at the grounding line of ice streams have consequences for inland ice dynamics and hence sea level. Despite substantial evidence documenting upstream propagation of frontal change, the mechanisms by...
5.
Mulvaney R, Abram N, Hindmarsh R, Arrowsmith C, Fleet L, Triest J, et al.
Nature
. 2012 Aug;
489(7414):141-4.
PMID: 22914090
Rapid warming over the past 50 years on the Antarctic Peninsula is associated with the collapse of a number of ice shelves and accelerating glacier mass loss. In contrast, warming...
6.
Arthern R, Hindmarsh R
Philos Trans A Math Phys Eng Sci
. 2006 Jun;
364(1844):1841-65.
PMID: 16782612
The problem of forecasting the future behaviour of the Antarctic ice sheet is considered. We describe a method for optimizing this forecast by combining a model of ice sheet flow...
7.
Hindmarsh R
Philos Trans A Math Phys Eng Sci
. 2006 Jun;
364(1844):1733-67.
PMID: 16782608
Membrane stresses act along thin bodies which are relatively well lubricated on both surfaces. They operate in ice sheets because the bottom is either sliding, or is much less viscous...