A. A. Variabilitévariabilit´variabilité and . Erou, u sont mesurées les niveaux de l'Amazone, car situéè a l'aval de la confluence des rios Marañón et Ucayali. A cette station, qui draine un bassin de 726 400 km 2 dont 53% situés dans les Andes, l'Amazone transporte de grandes quantités de sédiments

. Le-bassin-versant-de-l, Amazonè a Tamshiyacu a ´ eté délimitédélimitéà partir du modèle numérique de terrain SRTM, selon une procédure semi?automatique, 2005.

. Les-niveaux-d, eau journaliers de l'Amazonè a la station hydrométrique de Tamshiyacu (4.00 ? S et 73.16 ? W) sont mesurés par lecture d'uné echelle limnimétrique 4

S. Fois-par-jour,-par-un-observateur-du, Service National de Météorologie et d'Hydrologie, www.senamhi.gob.pe) depuis 1983. A cette station, une courbe d'´ etalonnage fiable a pû etre construire par le programme HYBAM (Fig. A.2), grâcè a 16 jaugeages réalisés de, par courantomètrè a effet Doppler (ADCP), techniqueparticulì erement bien adaptée aux grands fleuves amazoniens (Filizola and Guyot, 2004.

L. Données-de-hauteurs-d, eau de la station d'Iquitos (3.71 ? S et 73.25 ? W) gérée par ENAPU Pérou (Entreprise Nationale des Ports, www.enapu.com.pe) depuis 1969, ont permis d'´ etendre la série des débits de Tamshiyacù a la période, pp.1969-2005

A. Figure, 4 ? Rio AmazonasàAmazonasà Tamshiyacu : débits mensuels pour la période, et précipitation moyenne sur le bassin de avec lignes de tendance, 1969.

. Ede, les valeurs annuelles (Fig. A.7) montrent une diminution nette des précipitations (?0.83% par an), comme des débits (-0.81% par an) Les débits annuels minimum et maximum décroissentdécroissentégalement sur la période, avec des valeurs respectives de -0.61% et -1.68%. Il faut cependant signaler que les pluies de 1964à1964à 1970 présentent une tendancè a l'augmentation, montrant que l'année 1970 pourrait ici aussi représenter une rupture dans la série comme cela a déjàdéjàété observé sur d'autres fleuves amazoniens Calì, 1970.

. Cutim, du fait de l'augmentation des pluiesàpluiesà cetté epoque, comme cela a ´ etéetéégalement confirmé par d'autresétudesautresétudes sur le bassin de l Aussi la décroissance observée sur la série 1970?1997, peutêtrepeutêtre le résultat de cette hydraulicité anormalementélevéeanormalementélevée des années 1970, d'une tendance généralè a la diminution des pluies et des débits dans la région, Les débits observésobservésà Tamshiyacu montrent des valeurs plusélevéesplusélevées durant la décennie des années, 1970.

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