Publications des scientifiques de l'IRD

Espinoza J. C., Ronchail J., Frappart F., Lavado W., Santini William, Guyot Jean-Loup. (2013). The major floods in the Amazonas river and tributaries (Western Amazon Basin) during the 1970-2012 period : a focus on the 2012 flood. Journal of Hydrometeorology, 14 (3), p. 1000-1008. ISSN 1525-755X.

Titre du document
The major floods in the Amazonas river and tributaries (Western Amazon Basin) during the 1970-2012 period : a focus on the 2012 flood
Année de publication
2013
Type de document
Article référencé dans le Web of Science WOS:000320300600019
Auteurs
Espinoza J. C., Ronchail J., Frappart F., Lavado W., Santini William, Guyot Jean-Loup
Source
Journal of Hydrometeorology, 2013, 14 (3), p. 1000-1008 ISSN 1525-755X
In this work, the authors analyze the origin of the extreme floods in the Peruvian Amazonas River during the 1970-2012 period, focusing on the recent April 2012 flooding (55 400 m(3) s(-1)). Several hydrological variables, such as rainfall, terrestrial water storage, and discharge, point out that the unprecedented 2012 flood is mainly related to an early and abundant wet season over the north of the basin. Thus, the peak of the Maranon River, the northern contributor of the Amazonas, occurred sooner than usual (in April instead of May), coinciding with the peak of the Ucayali River, the southern contributor. This concomitance caused a dramatic flood downstream in the Peruvian Amazonas. These results are compared to the amplitude and timing of the three most severe extreme floods (1970-2011). The analysis of the climatic features related to the most important floods (1986, 1993, 1999, and 2012) suggests that they are characterized by a La Nina event, which originates a geopotential height wave train near the ground, with positive anomalies over the subtropical South and North Pacific and Atlantic and over southeastern South America. These patterns contribute to 1) the origin of an abundant humidity transport flux from the tropical North Atlantic and the Caribbean Sea toward the northwestern Amazon and 2) the maintenance of the monsoon flux over this region. They both favor a strong convergence of humidity in the northern Amazonas basin. Finally, the authors suggest that the intensity of floods is more likely related to an early La Nina event (as observed during the 2011/12 season), early rainfall, and simultaneous peaks of both tributaries of the Amazonas River.
Plan de classement
Sciences du milieu [021] ; Hydrologie [062]
Description Géographique
PEROU ; AMAZONIE
Localisation
Fonds IRD [F B010059907]
Identifiant IRD
fdi:010059907
Contact