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humidité spécifique (g/kg) en fonction de la température moyenne ( ? C) La ligne du dessus représente l'erreur résultant d'une erreur de température de, p.29, 1999. ,
pour un cas instable (gauche) et stable (droite), correspondant respectivementàrespectivementà une différence de température air/meràmerà 10m de +5 et -5 ? C (T s ´ etant fixéfixéà 15 ? C). L'humidité spécifique de l'airàairà 10métant10métant calculée pour correspondrè a une humidité relative, Coefficients de transferts bulk pour différentes paramétrisations en fonction du module du vent relatifàrelatifà 10m, p.86 ,
Ces climatologies ontétéontété construitesàconstruitesà partir des mêmes VEAS issues du DFS4 (chap. 8) et d'une SST inter-annuelle fixée, Désaccord moyen entre les climatologies de tension de vent estimées grâce aux algorithmes bulk COA3 et LY04, p.89, 1984. ,
Ces climatologies ontétéontété construitesàconstruitesà partir des mêmes VEAS issues du DFS4 (chap. 8) et d'une SST inter-annuelle fixée, p.89, 2007. ,
Fréquence d'occurrence (en %) de conditions stables durant la période 1984-2000 estimés grâcè a la longueur de Monin-Obukhov calculéè a partir des VEAS issues du DFS4 (chap. 8) et d'une SST inter-annuelle fixée, p.93, 2007. ,
des flux de chaleur latente (a) et sensible (b) estimées grâce ` a l'algorithme bulk LY04àLY04à partir des VEAS issues du DFS4 (chap. 8) et d'une SST inter-annuelle fixée, Climatologies, p.94, 1984. ,
) estimés grâce ` a l'algorithme bulk LY04àLY04à partir des VEAS issues du DFS4 (chap. 8) et de la SST inter-annuelle de, Profils zonaux des flux de chaleur latente et sensibles moyens, p.96, 1984. ,
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Amérique du sud, ERA-40 (a) et NCEP (b) Chacun de ces champs est représenté sur sa grille d'origine, 1.125 ? pour ERA-40 contre 1.875 ? pour NCEP. Le phénomène de Gibbs est observé pour le champ ERA-40 sur la côte ouest entre 30 ? S et 10 ? S mais son extension vers le large est faible, NCEP, en revanche, semble propager des perturbations beaucoup plus au large et demanì ere plus prononcée. . . . . . . . . . . . . . . . . . . . . . . . 115, 2000. ,
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Maillage et masque des points T en surface dans le Pacifique. (Avec l'aimable autorisation de Dr. F. Castruccio), p.129 ,