Circulation characteristics in three eddy-permitting models of the North Atlantic

A systematic intercomparison of three realistic eddy-permitting models of the North Atlantic circulation has been performed. The models use different concepts for the discretization of the vertical coordinate, namely geopotential levels, isopycnal layers, terrain-following (sigma) coordinates, respe...

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Bibliographic Details
Main Authors: Willebrand, Jürgen (Author), Barnier, Bernard (Author), Böning, Claus (Author), Dieterich, Christian (Author), Killworth, Peter D. (Author), Le Provost, Christian (Author), Jia, Yanli (Author), Molines, Jean-Marc (Author), New, Adrian L. (Author)
Format: Article
Language:English
Published: 2001.
Subjects:
Online Access:Get fulltext
LEADER 01683 am a22002173u 4500
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042 |a dc 
100 1 0 |a Willebrand, Jürgen  |e author 
700 1 0 |a Barnier, Bernard  |e author 
700 1 0 |a Böning, Claus  |e author 
700 1 0 |a Dieterich, Christian  |e author 
700 1 0 |a Killworth, Peter D.  |e author 
700 1 0 |a Le Provost, Christian  |e author 
700 1 0 |a Jia, Yanli  |e author 
700 1 0 |a Molines, Jean-Marc  |e author 
700 1 0 |a New, Adrian L.  |e author 
245 0 0 |a Circulation characteristics in three eddy-permitting models of the North Atlantic 
260 |c 2001. 
856 |z Get fulltext  |u https://eprints.soton.ac.uk/271/1/NEW_overview.pdf 
520 |a A systematic intercomparison of three realistic eddy-permitting models of the North Atlantic circulation has been performed. The models use different concepts for the discretization of the vertical coordinate, namely geopotential levels, isopycnal layers, terrain-following (sigma) coordinates, respectively. Although these models were integrated under nearly identical conditions, the resulting large-scale model circulations show substantial differences. The results demonstrate that the large-scale thermohaline circulation is very sensitive to the model representation of certain localised processes, in particular to the amount and water mass properties of the overflow across the Greenland-Scotland region, to the amount of mixing within a few hundred kilometers south of the sills, and to several other processes at small or sub-grid scales. The different behaviour of the three models can to a large extent be explained as a consequence of the different model representation of these processes. 
655 7 |a Article