The Major Floods in the Amazonas River and Tributaries (Western Amazon Basin) during the 1970-2012 Period: A Focus on the 2012 Flood

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 (55400m3 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 Marañón 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 Ni~na 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 Niña event (as observed during the 2011/12 season), early rainfall, and simultaneous peaks of both tributaries of the Amazonas River.

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Main Authors: Espinoza, J.C., Ronchail, J., Frappart, F., Lavado-Casimiro, W., Santini, W., Guyot, J.L.
Format: info:eu-repo/semantics/article biblioteca
Language:eng
Published: American Meteorological Society
Subjects:Amplitude, Flooding, Geopotential, Monsoon, Rainfall, Rios,
Online Access:https://hdl.handle.net/20.500.12542/63
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spelling dig-senamhi-pe-20.500.12542-632021-03-16T23:51:02Z The Major Floods in the Amazonas River and Tributaries (Western Amazon Basin) during the 1970-2012 Period: A Focus on the 2012 Flood Espinoza, J.C. Ronchail, J. Frappart, F. Lavado-Casimiro, W. Santini, W. Guyot, J.L. Amplitude Flooding Geopotential Monsoon Rainfall Rios 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 (55400m3 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 Marañón 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 Ni~na 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 Niña event (as observed during the 2011/12 season), early rainfall, and simultaneous peaks of both tributaries of the Amazonas River. 2013 info:eu-repo/semantics/article https://hdl.handle.net/20.500.12542/63 eng info:eu-repo/semantics/openAccess Atribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América application/pdf application/pdf American Meteorological Society Servicio Nacional de Meteorología e Hidrología del Perú Repositorio Institucional - SENAMHI
institution SENAMHI PE
collection DSpace
country Perú
countrycode PE
component Bibliográfico
access En linea
databasecode dig-senamhi-pe
tag biblioteca
region America del Sur
libraryname Biblioteca del SENAMHI Perú
language eng
topic Amplitude
Flooding
Geopotential
Monsoon
Rainfall
Rios
Amplitude
Flooding
Geopotential
Monsoon
Rainfall
Rios
spellingShingle Amplitude
Flooding
Geopotential
Monsoon
Rainfall
Rios
Amplitude
Flooding
Geopotential
Monsoon
Rainfall
Rios
Espinoza, J.C.
Ronchail, J.
Frappart, F.
Lavado-Casimiro, W.
Santini, W.
Guyot, J.L.
The Major Floods in the Amazonas River and Tributaries (Western Amazon Basin) during the 1970-2012 Period: A Focus on the 2012 Flood
description 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 (55400m3 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 Marañón 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 Ni~na 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 Niña event (as observed during the 2011/12 season), early rainfall, and simultaneous peaks of both tributaries of the Amazonas River.
format info:eu-repo/semantics/article
topic_facet Amplitude
Flooding
Geopotential
Monsoon
Rainfall
Rios
author Espinoza, J.C.
Ronchail, J.
Frappart, F.
Lavado-Casimiro, W.
Santini, W.
Guyot, J.L.
author_facet Espinoza, J.C.
Ronchail, J.
Frappart, F.
Lavado-Casimiro, W.
Santini, W.
Guyot, J.L.
author_sort Espinoza, J.C.
title The Major Floods in the Amazonas River and Tributaries (Western Amazon Basin) during the 1970-2012 Period: A Focus on the 2012 Flood
title_short The Major Floods in the Amazonas River and Tributaries (Western Amazon Basin) during the 1970-2012 Period: A Focus on the 2012 Flood
title_full The Major Floods in the Amazonas River and Tributaries (Western Amazon Basin) during the 1970-2012 Period: A Focus on the 2012 Flood
title_fullStr The Major Floods in the Amazonas River and Tributaries (Western Amazon Basin) during the 1970-2012 Period: A Focus on the 2012 Flood
title_full_unstemmed The Major Floods in the Amazonas River and Tributaries (Western Amazon Basin) during the 1970-2012 Period: A Focus on the 2012 Flood
title_sort major floods in the amazonas river and tributaries (western amazon basin) during the 1970-2012 period: a focus on the 2012 flood
publisher American Meteorological Society
url https://hdl.handle.net/20.500.12542/63
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