The role of the Amazon Basin moisture in the atmospheric branch of the hydrological cycle: a Lagrangian analysis

We used a Lagrangian model (FLEXPART) together with the 1979–2012 ERA-Interim reanalysis data to investigate the role of the moisture in the Amazon Basin in the regional hydrological budget over the course of the year. FLEXPART computes budgets of evaporation minus precipitation by calculating chang...

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Main Authors: A. Drumond, J. Marengo, T. Ambrizzi, R. Nieto, L. Moreira, L. Gimeno
Format: Article
Language:English
Published: Copernicus Publications 2014-07-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/18/2577/2014/hess-18-2577-2014.pdf
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author A. Drumond
J. Marengo
T. Ambrizzi
R. Nieto
L. Moreira
L. Gimeno
author_facet A. Drumond
J. Marengo
T. Ambrizzi
R. Nieto
L. Moreira
L. Gimeno
author_sort A. Drumond
collection DOAJ
description We used a Lagrangian model (FLEXPART) together with the 1979–2012 ERA-Interim reanalysis data to investigate the role of the moisture in the Amazon Basin in the regional hydrological budget over the course of the year. FLEXPART computes budgets of evaporation minus precipitation by calculating changes in the specific humidity along forward and backward trajectories. The tropical Atlantic is the most important remote moisture source for the Amazon Basin. The tropical North Atlantic (NA) mainly contributed during the austral summer, while the contribution of the tropical South Atlantic (SA) prevailed for the remainder of the year. At the same time, the moisture contribution from the Amazon Basin itself is mainly for moisture supplying the southeastern South America. The 33-year temporal domain allowed the investigation of some aspects of the interannual variability of the moisture transport over the basin, such as the role of the El Niño Southern Oscillation (ENSO) and the Atlantic Meridional Mode (AMM) on the hydrological budget. During the peak of the Amazonian rainy season (from February to May, FMAM) the AMM is associated more with the interannual variations in the contribution from the tropical Atlantic sources, while the transport from the basin towards the subtropics responds more to the ENSO variability. The moisture contribution prevailed from the SA (NA) region in the years dominated by El Niño/positive AMM (La Niña/negative AMM) conditions. The transport from the Amazon towards the subtropics increased (reduced) during El Niño (La Niña) years.
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spelling doaj.art-f2a364e79f6a4b1ab4d7fe9fa0977be72022-12-22T01:03:40ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382014-07-011872577259810.5194/hess-18-2577-2014The role of the Amazon Basin moisture in the atmospheric branch of the hydrological cycle: a Lagrangian analysisA. Drumond0J. Marengo1T. Ambrizzi2R. Nieto3L. Moreira4L. Gimeno5Ephyslab, Facultad de Ciencias, UVIGO, Ourense, SpainCCST INPE, Cachoeira Paulista, Sao Paulo, BrazilInstituto de Astronomia, Geofisica e Ciencias Atmosfericas, USP, Sao Paulo, BrazilEphyslab, Facultad de Ciencias, UVIGO, Ourense, SpainInstitute of Applied Physics, University of Bern, Bern, SwitzerlandEphyslab, Facultad de Ciencias, UVIGO, Ourense, SpainWe used a Lagrangian model (FLEXPART) together with the 1979–2012 ERA-Interim reanalysis data to investigate the role of the moisture in the Amazon Basin in the regional hydrological budget over the course of the year. FLEXPART computes budgets of evaporation minus precipitation by calculating changes in the specific humidity along forward and backward trajectories. The tropical Atlantic is the most important remote moisture source for the Amazon Basin. The tropical North Atlantic (NA) mainly contributed during the austral summer, while the contribution of the tropical South Atlantic (SA) prevailed for the remainder of the year. At the same time, the moisture contribution from the Amazon Basin itself is mainly for moisture supplying the southeastern South America. The 33-year temporal domain allowed the investigation of some aspects of the interannual variability of the moisture transport over the basin, such as the role of the El Niño Southern Oscillation (ENSO) and the Atlantic Meridional Mode (AMM) on the hydrological budget. During the peak of the Amazonian rainy season (from February to May, FMAM) the AMM is associated more with the interannual variations in the contribution from the tropical Atlantic sources, while the transport from the basin towards the subtropics responds more to the ENSO variability. The moisture contribution prevailed from the SA (NA) region in the years dominated by El Niño/positive AMM (La Niña/negative AMM) conditions. The transport from the Amazon towards the subtropics increased (reduced) during El Niño (La Niña) years.http://www.hydrol-earth-syst-sci.net/18/2577/2014/hess-18-2577-2014.pdf
spellingShingle A. Drumond
J. Marengo
T. Ambrizzi
R. Nieto
L. Moreira
L. Gimeno
The role of the Amazon Basin moisture in the atmospheric branch of the hydrological cycle: a Lagrangian analysis
Hydrology and Earth System Sciences
title The role of the Amazon Basin moisture in the atmospheric branch of the hydrological cycle: a Lagrangian analysis
title_full The role of the Amazon Basin moisture in the atmospheric branch of the hydrological cycle: a Lagrangian analysis
title_fullStr The role of the Amazon Basin moisture in the atmospheric branch of the hydrological cycle: a Lagrangian analysis
title_full_unstemmed The role of the Amazon Basin moisture in the atmospheric branch of the hydrological cycle: a Lagrangian analysis
title_short The role of the Amazon Basin moisture in the atmospheric branch of the hydrological cycle: a Lagrangian analysis
title_sort role of the amazon basin moisture in the atmospheric branch of the hydrological cycle a lagrangian analysis
url http://www.hydrol-earth-syst-sci.net/18/2577/2014/hess-18-2577-2014.pdf
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