Villar J.C.E. auteur aut IRD Ronchail J. auteur aut IRD Guyot Jean-Loup auteur aut IRD Cochonneau Gérard auteur aut IRD Naziano F. auteur aut IRD Lavado W. auteur aut IRD De Oliveira E. auteur aut IRD Pombosa R. auteur aut IRD Vauchel Philippe auteur aut IRD text journalArticle eng text/pdf born digital access Rainfall variability in the Amazon basin (AB) is analysed for the 1964-2003 period. It is based on 756 pluviometric stations distributed throughout the AB countries. For the first time it includes data from Bolivia, Peru, Ecuador, and Colombia. In particular, the recent availability of rainfall data from the Andean countries makes it possible to complete previous studies. The impact Of Mountain ranges oil rainfall is pointed out. The highest rainfall ill the AB is observed in low windward regions, and low rainfall is measured in leeward and elevated stations. Additionally, rainfall regimes are more diversified in the Andean regions than in the lowlands. Rainfall spatio-temporal variability is studied based on a varimax-rotated principal component analysis (PCA). Long-term variability with a decreasing rainfall since the 1980s prevails in June-July-August (JJA) and September-October-November (SON). During, the rainiest seasons, i.e. December-January-February (DJF) and March-April-May (MAM), the main variability is at decadal and interannual time scales. Interdecadal variability is related to long-term changes in the Pacific Ocean, whereas decadal variability, opposing the northwest and the south of the AB, is associated with changes in the strength of the low-level jet (LLJ) along the Andes. Interannual variability characterizes more specifically the northeast of the basin and the southern tropical Andes. It is related to El Nino-Southern Oscillation (ENSO) and to the sea surface temperature (SST) gradient over the tropical Atlantic. Mean rainfall in the basin decreases during the 1975-2003 period at an annual rate estimated to be -0.32%. Break tests show that this decrease has been particularly important since 1982. Further insights into this phenomenon will permit to identify the impact of climate on the hydrology of the AB. specialized rainfall variability rainfall regimes Amazon basin Andes South American climate Peru Ecuador Bolivia Colombia ENSO PDO LLJ 062 021 29 11 1574-1594 2009 0899-8418 https://www.documentation.ird.fr/hor/fdi:010048193 10.1002/joc.1791 0899-8418 [F B010048193] https://www.documentation.ird.fr/hor/fdi:010048193 https://www.documentation.ird.fr/intranet/publi/2009/10/010048193.pdf Accès réservé (Intranet de l'IRD) IRD - Base Horizon / Pleins textes 2009-11-09 2017-08-23 fdi:010048193 fre