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.. .. Conclusions,

, L'approche numérique semi-idéalisée offre la possibilité de tester uneà une les influences de

, Analyse de phénomènes clés pour la qualité de l'air

, En effet, comme nous l'avons vu dans la section 6.3.3, la trajectoire du DVW résulte d'interactions multiples entre lesécoulements en provenance des différentes vallées tributaires. Des analyses supplémentaires seraient donc nécessaires

, U) et méridienne (V) du vent calculéssur les périodes (a-b) stable et (c-d) convective avec la méthode que ceux présentés sur la Figure 7.6. En journée, le UVW (apparentéà la composante U) apparaît plus intense et plus développé verticalement sur les simulations SWmar LS et SWmar VS, Figure 7.10 -Profils verticaux moyens des composantes zonale

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