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Fausto Ferraccioli

Researcher at British Antarctic Survey

Publications -  134
Citations -  5943

Fausto Ferraccioli is an academic researcher from British Antarctic Survey. The author has contributed to research in topics: Antarctic ice sheet & Ice sheet. The author has an hindex of 33, co-authored 126 publications receiving 4690 citations. Previous affiliations of Fausto Ferraccioli include University of Genoa & Natural Environment Research Council.

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Bedmap2: improved ice bed, surface and thickness datasets for Antarctica

Peter T. Fretwell, +59 more
- 28 Feb 2013 - 
TL;DR: Bedmap2 as discussed by the authors is a suite of gridded products describing surface elevation, ice-thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60° S. In particular, the Bedmap2 ice thickness grid is made from 25 million measurements, over two orders of magnitude more than were used in Bedmap1.
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Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet

TL;DR: In this paper, a high-resolution and physically based description of Antarctica bed topography using mass conservation is presented, revealing previously unknown basal features with major implications for glacier response to climate change.
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East Antarctic rifting triggers uplift of the Gamburtsev Mountains

TL;DR: The evolution of the Gamburtsevs demonstrates that rifting and preserved orogenic roots can produce broad regions of high topography in continental interiors without significantly modifying the underlying Precambrian lithosphere.
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New boundary conditions for the West Antarctic ice sheet: Subglacial topography beneath Pine Island Glacier

TL;DR: In this paper, an improved subglacial topography for the Pine Island Glacier basin has been derived, and the trunk of this glacier lies in a narrow, 250-km long, 500m deep sub-glacial trough, suggesting a longlived and constrained ice stream.
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Evidence from ice shelves for channelized meltwater flow beneath the Antarctic Ice Sheet

TL;DR: In this paper, remote sensing observations reveal persistent channelized features beneath the Filchner-Ronne Ice Shelf in West Antarctica, suggesting widespread channelized flow driven by melting.