@Article{DrumondMaAmNiMoGi:2014:LaAn,
author = "Drumond, A. and Marengo, Jos{\'e} Antonio and Ambrizzi, T. and
Nieto, R. and Moreira, L. and Gimeno, L.",
affiliation = "UVIGO and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidade de S{\~a}o Paulo (USP)} and UVIGO and {University
of Bern} and UVIGO",
title = "The role of the Amazon Basin moisture in the atmospheric branch of
the hydrological cycle: A Lagrangian analysis",
journal = "Hydrology and Earth System Sciences",
year = "2014",
volume = "18",
number = "7",
pages = "2577--2598",
keywords = "Atmospheric humidity, Atmospheric pressure, Budget control,
Lagrange multipliers, Moisture, Forward-and-backward, Hydrological
budgets, Hydrological cycles, Interannual variability, Interannual
variation, Lagrangian analysis, Southeastern South America,
Southern oscillation, Tropics, El Nino, El Nino-Southern
Oscillation, evaporation, hydrological cycle, Lagrangian analysis,
moisture transfer, precipitation (climatology), water budget,
Amazon Basin, Atlantic Ocean, Atlantic Ocean (North), Atlantic
Ocean (South), Atlantic Ocean (Tropical).",
abstract = "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 Niņo 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 Niņo/positive AMM (La
Niņa/negative AMM) conditions. The transport from the Amazon
towards the subtropics increased (reduced) during El Niņo (La
Niņa) years.",
doi = "10.5194/hess-18-2577-2014",
url = "http://dx.doi.org/10.5194/hess-18-2577-2014",
issn = "1027-5606",
label = "scopus 2014-11 DrumondMaAmNiMoGi:2014:LaAn",
language = "en",
targetfile = "Drumond_role.pdf",
urlaccessdate = "27 abr. 2024"
}