E
Eric Deleersnijder
Researcher at Université catholique de Louvain
Publications - 253
Citations - 7666
Eric Deleersnijder is an academic researcher from Université catholique de Louvain. The author has contributed to research in topics: Finite element method & Discontinuous Galerkin method. The author has an hindex of 45, co-authored 250 publications receiving 6954 citations. Previous affiliations of Eric Deleersnijder include Delft University of Technology & University of Liège.
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Journal ArticleDOI
Carbon and nitrogen cycling within the Bering/Chukchi Seas: Source regions for organic matter effecting AOU demands of the Arctic Ocean
John J. Walsh,C. P. McRoy,L. K. Coachman,John J. Goering,Jacques Nihoul,Terry E. Whitledge,T. H. Blackburn,P. L. Parker,Creighton D. Wirick,P. G. Shuert,Jacqueline M. Grebmeier,Jacqueline M. Grebmeier,Alan M. Springer,R. D. Tripp,Dennis A. Hansell,Salim Djenidi,Eric Deleersnijder,K. Henriksen,B. A. Lund,P. Andersen,Frank E. Muller-Karger,Frank E. Muller-Karger,Kenneson G. Dean +22 more
TL;DR: In this article, the authors present a survey of the state-of-the-art marine science institutions in the United States, including the University of Alaska, Fairbanks, Alaska 99701, U.S.
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The concept of age in marine modelling I. Theory and preliminary model results
TL;DR: In this article, an Eulerian theory of the age is presented, in which advection, diffusion, production and destruction phenomena are properly accounted for, and the mean age of a set of particles is evaluated as the mass-weighted average of the ages of the particles under study.
Journal ArticleDOI
Lagrangian ocean analysis: Fundamentals and practices
Erik van Sebille,Erik van Sebille,Stephen M. Griffies,Ryan Abernathey,Thomas P. Adams,Pavel Berloff,Arne Biastoch,Bruno Blanke,Eric P. Chassignet,Yu Cheng,Colin J. Cotter,Eric Deleersnijder,Eric Deleersnijder,Kristofer Döös,Henri F. Drake,Henri F. Drake,Sybren Drijfhout,Stefan F. Gary,Arnold Heemink,Joakim Kjellsson,Joakim Kjellsson,Inga Monika Koszalka,Michael Lange,Camille Lique,G. A. MacGilchrist,Robert Marsh,C. Gabriela Mayorga Adame,Ronan McAdam,Francesco Nencioli,Claire B. Paris,Matthew D. Piggott,Jeff A. Polton,Siren Rühs,Syed Hyder Ali Muttaqi Shah,Syed Hyder Ali Muttaqi Shah,Matthew D. Thomas,Jinbo Wang,Phillip J. Wolfram,Laure Zanna,Jan D. Zika,Jan D. Zika +40 more
TL;DR: Lagrangian analysis is a powerful way to analyse the output of ocean circulation models and other ocean velocity data such as from altimetry as mentioned in this paper, where large sets of virtual particles are integrated within the 3D, time-evolving velocity fields.
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Description of the Earth system model of intermediate complexity LOVECLIM version 1.2
Hugues Goosse,V. Brovkin,Thierry Fichefet,Reindert J. Haarsma,Philippe Huybrechts,JI Jongma,Anne Mouchet,Frank Selten,Pierre-Yves Barriat,Jean-Michel Campin,Eric Deleersnijder,Emmanualle Driesschaert,Heiko Goelzer,I. Janssens,Marie-France Loutre,M. A. Morales Maqueda,Theo Opsteegh,P.-P. Mathieu,Guy Munhoven,E. J. Pettersson,Hans Renssen,Didier M. Roche,Didier M. Roche,Michiel Schaeffer,B. Tartinville,Axel Timmermann,S. L. Weber +26 more
TL;DR: LOVECLIM 1.2 as discussed by the authors is a 3D Earth system model of intermediate complexity, which includes representations of the atmosphere, the ocean and sea ice, the land surface (including vegetation), the ice sheets, the icebergs and the carbon cycle.
Description of the Earth system model of intermediate complexity LOVECLIM version 1.2
Hugues Goosse,Victor Brovkin,Thierry Fichefet,Reindert J. Haarsma,Philippe Huybrechts,JI Jongma,Anne Mouchet,F. Selton,Pierre-Yves Barriat,M.-L. Campin,Eric Deleersnijder,E. Driesschaert,Heiko Goelzer,I. Janssens,Marie-France Loutre,M. A. Morales Maqueda,Theo Opsteegh,P.-P. Mathieu,Guy Munhoven,E. J. Pettersson,Hans Renssen,Didier M. Roche,Michiel Schaeffer,B. Tartinville,Axel Timmermann,S. L. Weber +25 more
TL;DR: The new version of the three-dimensional Earth system model of intermediate complexity LOVECLIM reproduces well the major characteristics of the observed climate both for present-day conditions and for key past periods such as the last millennium, the mid-Holocene and the Last Glacial Maximum, but some biases are still present in the model.