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 ,
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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. ,
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 ,
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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. ,
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