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est une chose de penser que l'on est sur le bon chemin, une autre de croire que ce chemin est le seul. De toute façon, ce sont toutes des façons, » Proverbe mexicain ,
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,
, 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
, 10-c et -d) met enévidence une redistribution desécoulements en réponse au forçage radiatif. Sous le forçage de février, la différence d'ensoleillement entre les versants Nord et Sud du bassin privilégie le développement d'une circulation perpendiculaireà l'axe du bassin (V>U dans les premiers 100m pour REF et SWfeb LS). Cette circulation favorise l'advection des traceurs le long du versant Nord.À l'inverse, le forçage radiatif de Mars ré-équilibre cette dissymétrie Nord-Sud et privilégie le développement de l, la comparaison des composantes journalières de U et V (panels 7
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