M
Mark Inall
Researcher at Scottish Association for Marine Science
Publications - 118
Citations - 4326
Mark Inall is an academic researcher from Scottish Association for Marine Science. The author has contributed to research in topics: Internal wave & Internal tide. The author has an hindex of 33, co-authored 108 publications receiving 3607 citations. Previous affiliations of Mark Inall include Bangor University & University of the Highlands and Islands.
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Water mass modification in an Arctic fjord through cross-shelf exchange: The seasonal hydrography of Kongsfjorden, Svalbard
TL;DR: In this article, the authors investigated the cross-shelf exchange processes in Kongsfjorden and the West Spitsbergen Shelf using conductivity-temperature-depth (CTD) observations from 2000-2003 and a 5-month mooring deployment through the spring and summer of 2002.
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A sea change in our view of overturning in the subpolar North Atlantic
M. S. Lozier,Feili Li,Sheldon Bacon,Frank Bahr,Amy S. Bower,Stuart A. Cunningham,M. F. de Jong,L. de Steur,Brad deYoung,Jürgen Fischer,Stefan F. Gary,Blair J. W. Greenan,Naomi P. Holliday,Adam Houk,Loïc Houpert,Mark Inall,Mark Inall,William E. Johns,Helen L. Johnson,Clare Johnson,Johannes Karstensen,G. Koman,I. A. A. Le Bras,Xiaopei Lin,Neill Mackay,David P. Marshall,Hugo Mercier,Marilena Oltmanns,Robert S. Pickart,Andree L. Ramsey,Darren Rayner,Fiammetta Straneo,Virginie Thierry,Daniel J. Torres,Richard G. Williams,Chris Wilson,Jiayan Yang,Igor Yashayaev,Jian Zhao +38 more
TL;DR: It is suggested that the conversion of warm, salty, shallow Atlantic waters into colder, fresher, deep waters that move southward in the Irminger and Iceland basins is largely responsible for overturning and its variability in the subpolar basin.
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Wintertime warming of an Arctic shelf in response to large‐scale atmospheric circulation
Finlo Cottier,Frank Nilsen,Frank Nilsen,Mark Inall,Sebastian Gerland,Vigdis Tverberg,Harald Svendsen +6 more
TL;DR: In this paper, the authors show that the dynamic response of the shelf to wind forcing has a profound effect on the heat content of the water, and that the winter temperature of the West Spitsbergen Shelf reverted to that typical of fall, interrupting the normal cycle of sea ice formation in the region.
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Calving rates at tidewater glaciers vary strongly with ocean temperature
TL;DR: It is found that frontal ablation is not dependent on ice dynamics, nor reduced by glacier surface freeze-up, but varies strongly with sub-surface water temperature, which illustrates the potential for deriving simple models of tidewater glacier response to oceanographic forcing.
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Does Presence of a Mid-Ocean Ridge Enhance Biomass and Biodiversity?
Imants G. Priede,Odd Aksel Bergstad,Peter I. Miller,Michael Vecchione,Andrey Gebruk,Tone Falkenhaug,David S.M. Billett,Jessica Craig,Andrew Dale,Mark A. Shields,Gavin H. Tilstone,Tracey T. Sutton,Andrew J. Gooday,Mark Inall,Daniel O.B. Jones,Victor Martinez-Vicente,Gui M. Menezes,Tomasz Niedzielski,Þorsteinn Sigurðsson,Nina Rothe,Antonina Rogacheva,Claudia H. S. Alt,Tim Brand,Richard Abell,Andrew S. Brierley,Nicola J. Cousins,Deborah Crockard,A. Rus Hoelzel,Åge S. Høines,Tom B. Letessier,J.F. Read,Tracy M Shimmield,Martin J. Cox,John K. Galbraith,John D M Gordon,Tammy Horton,Francis Neat,Pascal Lorance +37 more
TL;DR: It is proposed that globally sea floor elevation has no effect on deep sea biomass; pelagic plus benthic biomass is constant within a given surface productivity regime.