A. L. Dernièrement, B. A. Ba, and E. E. , 07 7) ) qui ont adapté l'approche énergétique en incluant l'influence du vent et des marées, ou Ces études mettent en valeur la précision des formules grâces à la comparaison des valeurs calculées avec des mesures réalisées sur le terrain, p.0

E. Sc, . Ho, D. N. On, . Da, and . I. Vi, ) voire même entre plusieurs modèles afin d'observer leur comportement réciproque, pp.19-99

E. E. , S. Sc, . Ho, H. N. On, A. Ha et al., Ces études concernent uniquement la modélisation du transport longitudinal or des expressions sont également utilisées pour modéliser le transport transversal, pp.19-99

C. Ca, A. St, . El, and . E. Le, Ces couplages hydrodynamiques et morphologiques ont également permis d'étudier la morphogénèse des barres pré-littorales aquitaines, 99900.

D. Da and A. Ou-u-e-et-t-a, ) ou d'étudier l'impact de tempêtes sur les plages méditerranéennes et du nord de la France

V. Vo and O. L. Ul, 19 99 94 4) ) sur le littoral estdunkerquois ou encore

A. L. Le and E. Vo-oy-y-e-et-t-a, 19 99 98 8) ) avaient également utilisé cette technique sur les côtes belges avec plus de succès puisqu'ils avaient pu déterminer l'intensité du transport sédimentaire

A. L. Le and E. Vo-oy-y-e-et-t, 08 8) ) sur les côtes de Charente-Maritime ou encore, p.0

L. Le and E. Vo-oy-y-e-et-t-a, utilisation de modèles ou de formules numériques permettant de déterminer le transport potentiel a été également très utilisée avec plus ou moins de vérification sur le terrain

A. L. Ab-b-)-)-sur-le-littoral-du-cotentin, S. Se, E. Dr, B. At-ti-i, M. Ma et al., ) ) sur le littoral de la côte d'Opale) ) sur l, 20 00 06 6) ), pp.99-94

K. and V. O. Vo, 19 97 72 2) ), la formation et la stabilité de ces formes sédimentaires ainsi que leurs migrations transversales successives sur l'estran reste un point récurent et fondamental très souvent abordé mais toujours pas complètement élucidé, 99922.

A. L. , S. St, and P. A. Ep, 19 99 98 8) ), 19 99 99 9) )

L. Vo-oy-y, K. Kr, W. O. Oo, . Wi, . Jn et al., 02 2) ), p.0

K. Kr, R. Oo-on-n, V. Va, A. N. Ho, . Uw et al., ) )

A. L. Ho and . Ny-y, ) ). Leur présence et leur mouvement à travers la zone intertidale attestent la présence d'un transport sédimentaire transversal essentiellement orienté

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.. Répartition-verticale-des-flux-sédimentaires-transversaux, 211 1.3.1. Caractérisation de la distribution verticale du transport sédimentaire transversal grâce au calcul du coefficient de décroissance Comparaison entre les profils de transport sédimentaire transversaux et les profils de vitesse au sein de la colonne d', ., p.215

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D. Des-ordres-de-grandeurs, 335 3.3. Deux composantes pour deux morphodynamiques bien distinctes, ., p.338