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16 | \vspace*{0.5cm} |
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17 | {\Large |
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18 | \begin{center} |
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19 | OASIS3\\ |
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20 | {\bf O}cean {\bf A}tmosphere {\bf S}ea {\bf I}ce {\bf S}oil\\ |
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21 | \vspace{0.4cm} |
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22 | User's Guide \\ |
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23 | \vspace{0.4cm} |
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24 | {\large oasis3\_prism\_2-2, June 2004} |
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25 | |
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26 | \end{center} |
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27 | } |
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28 | |
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29 | \vspace*{1cm} |
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30 | |
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31 | \centerline{Sophie Valcke$^1$, Arnaud Caubel$^2$, Reiner |
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32 | Vogelsang$^3$, Damien Declat$^1$} |
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33 | |
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34 | \vspace*{1cm} |
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35 | \centerline{PRISM Project WP3a} |
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36 | \centerline{$^1$C.E.R.F.A.C.S.} |
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37 | \centerline{$^2$FECIT/Fujitsu} |
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38 | \centerline{$^3$SGI Germany} |
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39 | |
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40 | \begin{abstract} |
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41 | This User's Guide contains a detailed step-by-step description on |
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42 | how to realize a coupled simulation with OASIS3. |
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43 | |
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44 | The aim of OASIS3 is to provide a flexible and user friendly tool |
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45 | for coupling independent |
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46 | general circulation models of the atmosphere and the ocean (A/O-GCMs) |
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47 | as well as other climate component models (sea-ice, land, |
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48 | atmospheric chemistry, ocean biogeochemistry, ...) and regional models. |
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49 | The resulting coupled models are necessary tools to tackle |
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50 | current climatic paradigms such as the natural variability, |
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51 | El Ni\~no Southern Oscillation |
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52 | (ENSO) or the greenhouse gas global warming effect. |
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53 | |
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54 | OASIS3 synchronizes the exchanges of coupling fields between |
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55 | the models being coupled, and performs |
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56 | 2D interpolations and transformations needed to express, on the grid |
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57 | of the target model, the coupling |
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58 | fields produced by the source model on its grid. Modularity and |
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59 | flexibility have been particularly emphasized in OASIS3 design. |
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60 | |
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61 | \end{abstract} |
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