C
Carol J. Pudsey
Researcher at British Antarctic Survey
Publications - 57
Citations - 5292
Carol J. Pudsey is an academic researcher from British Antarctic Survey. The author has contributed to research in topics: Ice sheet & Continental shelf. The author has an hindex of 35, co-authored 57 publications receiving 4957 citations. Previous affiliations of Carol J. Pudsey include Natural Environment Research Council.
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Journal ArticleDOI
Recent Rapid Regional Climate Warming on the Antarctic Peninsula
David G. Vaughan,Gareth J. Marshall,William M. Connolley,Claire L. Parkinson,Robert Mulvaney,Dominic A. Hodgson,John C. King,Carol J. Pudsey,John Turner +8 more
TL;DR: In this paper, the authors discuss the significance of rapid regional (RRR) warming in one area, the Antarctic Peninsula, and discuss several possible candidate mechanisms: changing oceanographic or changing atmospheric circulation, or a regional air-sea-ice feedback amplifying greenhouse warming.
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Bottom currents, contourites and deep-sea sediment drifts: current state-of-the-art
TL;DR: The Atlas of Contourite Systems (Atlas of contourite systems) as discussed by the authors has been used as a reference for bottom currents, contourites, and drifts.
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Flow dynamics and till genesis associated with a marine-based Antarctic palaeo-ice stream.
Colm Ó Cofaigh,Julian A. Dowdeswell,Claire S. Allen,John F. Hiemstra,Carol J. Pudsey,Jeffrey Evans,David J.A. Evans +6 more
TL;DR: In this paper, the authors show that during the last glacial cycle a palaeo-ice stream drained the Antarctic Peninsula Ice Sheet (APIS) through Marguerite Bay to the edge of the continental shelf via a bathymetric trough (Marguerite Trough).
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Evolution of subglacial bedforms along a paleo-ice stream, Antarctic Peninsula continental shelf
TL;DR: In this article, geophysical data from the Antarctic Peninsula continental shelf reveal streamlined subglacial bedforms in a cross-shelf trough, which exhibit progressive elongation with distance along the trough, and record flow of a paleo-ice stream from the Antarctica Peninsula Ice Sheet during the last glacial maximum.
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Thickness and extent of the subglacial till layer beneath an Antarctic paleo–ice stream
TL;DR: In this article, the authors reconstructed the thickness of the sedimentary bed under a large Antarctic paleo-ice stream for the first time, showing that fast flow is indicated by streamlined seafloor lineations that form the surface of a layer of low shear strength, unsorted sediment, averaging 4.6 m thick.