B
Bernard Coakley
Researcher at University of Alaska Fairbanks
Publications - 66
Citations - 4186
Bernard Coakley is an academic researcher from University of Alaska Fairbanks. The author has contributed to research in topics: Arctic & Seafloor spreading. The author has an hindex of 28, co-authored 62 publications receiving 3730 citations. Previous affiliations of Bernard Coakley include Columbia University & Tulane University.
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The International Bathymetric Chart of the Arctic Ocean (IBCAO) Version 3.0
Martin Jakobsson,Larry A. Mayer,Bernard Coakley,Julian A. Dowdeswell,Steve Forbes,Boris Fridman,Hanne Hodnesdal,Riko Noormets,Richard Pedersen,Michele Rebesco,Hans Werner Schenke,Yulia Zarayskaya,Daniela Accettella,Andy Armstrong,Robert M Anderson,Paul Bienhoff,Angelo Camerlenghi,I. Church,Margo H. Edwards,James V. Gardner,John K. Hall,Benjamin Hell,Ole Hestvik,Yngve Kristoffersen,Christian Marcussen,Rezwan Mohammad,David C. Mosher,Son V. Nghiem,Maria T. Pedrosa,Paola Travaglini,Pauline Weatherall +30 more
TL;DR: The International Bathymetric Chart of the Arctic Ocean (IBCAO) released its first gridded bathymetric compilation in 1999 as discussed by the authors, which has since supported a wide range of Arc...
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New grid of Arctic bathymetry aids scientists and mapmakers
TL;DR: For over two decades, Sheet 5.17 of the Fifth Edition of the General Bathymetric Chart of the Oceans (GEBCO) [Canadian Hydrographic Service, 1979] has been considered the authoritative portrayal of the sea floor north of 64 N as discussed by the authors.
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Simulation of Foreland Basin Stratigraphy using a diffusion model of mountain belt uplift and erosion: An example from the central Alps, Switzerland
TL;DR: In this paper, the authors present a simple model of three interacting processes: thrust deformation, sedimentary and erosional processes which redistribute that load, and the flexural response of the lithosphere.
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A model for the headward erosion of submarine canyons induced by downslope-eroding sediment flows
TL;DR: In this article, a simple, physically-based computer model of continental slope evolution is used to investigate the sequence of submarine canyon formation, which simulates submarine canyons as evolving under the influence of sedimentation, slope failure, sediment flow erosion, and topography.
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Ice shelves in the Pleistocene Arctic Ocean inferred from glaciogenic deep-sea bedforms
TL;DR: Backscatter images and sub-bottom profiler records obtained during the submarine SCICEX expedition in 1999 show multiple bedforms indicative of glacial scouring and moulding of sea floor, combined with large-scale erosion of submarine ridge crests, demonstrating that immense, Antarctic-type ice shelves existed in the Arctic Ocean during Pleistocene glaciations.