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. De-janvier, estran inférieur qui subit un exhaussement de l'ordre de 20 à 30 cm. En revanche à partir de janvier 2005, le profil montre une tendance claire à l'érosion. Entre janvier le profil subit une érosion importante qui se produit à la fois au niveau de l'estran inférieur et supérieur, 2000.

. Entre-juin, estran inférieur continue de s'éroder, avec une perte d'épaisseur de l'ordre de 20 cm observable à partir de 10 m (distance cross-shore) Au niveau de l'estran supérieur, un talus d'érosion de 20 cm de hauteur est perceptible sur le profil de décembre 2012. Il est possible que celui-ci était déjà présent antérieurement mais qu, 2010.

. De-décembre, la variabilité morphologique du profil est plus significative au niveau de l'estran supérieur Entre décembre 2013 et décembre 2014, l'affouillement du haut de plage se poursuit, signalé par le talus d'érosion dont la hauteur atteint 65 cm en décembre 2014. En décembre 2015, le talus n'est plus visible mais la forte concavité du, 2012.

. Le-bilan-volumique-de-ce-profil-montre-qu-'entre, la tendance est à l'érosion avec un taux moyen de -0,77 m 3 /an (R 2 VVF(1)=0,72) (Figure 6-25). La tendance d'évolution est encore plus significative sur la période de, pp.35-38, 2000.

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