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R. Ecarts, en cm) par rapportàrapport`rapportà la topographie dynamique (SLA + MDT) pour la simulation libre (en vert) et les expériences avec assimilation de données EXP2 (en bleu) et EXP3 (en rouge) et EXP4 (en noir), p.117

R. Ecarts and @. En, par rapport aux profils de température TAO pour la simulation libre (en vert) et les expériences avec assimilation de données EXP2 (en bleu), EXP3 (en rouge) et EXP4 (en noir), p.118

. Evolution-temporelle-de-la-dtàdt, DTà l'´ equateuràequateur`equateurà 156 ? E de longitude de la simulation assimilant la topographie dynamique (en bleu), de la simulation assimilant les TAO (en rouge) et de la simulation assimilant conjointement la topographie dynamique et les TAO (en noir). L'´ evolution temporelle de la hauteur dynamique déduite des TAO au même point est tracée (en magenta ), p.120

. .. Profil-de-température-tracés, droite) moyen pour l'année 1993 au point 0 ? N-156 ? E. Les profils des observations TAO (en magenta), de la simulation assimilant la topographie dynamique (en bleu), de la simulation assimilant les TAO (en rouge) et de la simulation assimilant conjointement la topographie dynamique, sont, p.120

R. Ecarts and @. C. En, par rapport aux profils de température TAO pour la simulation libre (en vert) et pour la simulation assimilée (en noir), p.137

R. Profils-d-'´-ecarts, en ? C) sur la verticale par rapport aux profils de température TAO (` a gauche) et par rapport aux profils de température XBTs indépendantes collectés par les navire VOS (` a droite) pour tout le Pacifique Tropical. Les RMSD pour la simulation libre (en vert) et pour la simulation assimilée (en noir) sont tracées, p.139

.. Ecart-type-de-température-le-long-de-l, ´ equateur et pour une section méridienneméridiennè a 155 ? W pour les observations TAO (en haut), la simulation libre (au milieu ) et la simulation avec assimilation de données (en bas) Les isocontours du champ moyen de température sont superposés, p.148

.. Et-panama-auckland, Central Pacific et East PacificéchantillonnéPacificéchantillonné demanì ereregulì ere par les navire VOS. Ces rails correspondent respectivement aux lignes maritimes Tokyo-Auckland, Position des rails West Pacific, p.149

. Transport-zonal-de-masse.., 10 6 m 3 s ?1 ) pour la couche de surface avec ? ? < 24kgm ?3 . Les vecteurs sont proportionnels au transport moyen dans la classe de densité pour chaque intervalle de 1 ? de latitude. Pour chaque année, le printemps boréal (en haut) et l'automne boréal (en bas), p.163

.. Transport-zonal-de-masse, s ?1 ) pour la couche intermédiaire avec 24 kg m ?3 < ? ? < 26.25 kg m ?3 . Les vecteurs sont proportionnels au transport moyen dans la classe de densité pour chaque intervalle de 1 ? de latitude. Pour chaque année, le printemps boréal (en haut) et l'automne boréal (en bas), p.168

.. Transport-zonal-de-masse, s ?1 ) pour la couche intermédiaire avec 24 kg m ?3 < ? ? < 26.25 kg m ?3 . Les vecteurs sont proportionnels au transport moyen dans la classe de densité pour chaque intervalle de 1 ? de latitude. Pour chaque année, le printemps boréal (en haut) et l'automne boréal (en bas), p.169

.. Transport-zonal-de-masse, s ?1 ) pour la couche intermédiaire avec 24 kg m ?3 < ? ? < 26.25 kg m ?3 . Les vecteurs sont proportionnels au transport moyen dans la classe de densité pour chaque intervalle de 1 ? de latitude. Pour chaque année, le printemps boréal (en haut) et l'automne boréal (en bas), p.170

H. Definition-of, 194 A.5 Mean surface current velocity for (a) the control run EXPT0, and the (b) EXPT1, p.2

B. 4. , M. Grace-mdts, and .. , ainsi que la MDT de la simulation non perturbée (au milieù a gauche) et la combinaison linéaire des MDTs issues de l'ensemble (au milieù a droite) En bas, carte des différences avec la MDT GRACE pour, respectivement, la MDT de la simulation non perturbée, p.209

C. Table-des-figures, 11 Spatial distribution of standard deviation error values on the latent heat flux (left-hand column) and the sensible heat flux (right-hand column) for V 0 (upper plots), V 1 (middle plots) and V 2 (bottom plots), p.232