@Article{LimbergerSiPeCaMaLi:2021:StPrTr,
author = "Limberger, Leila and Silva, Maria Elisa Siqueira and Pereira,
Gabriel and Cardozo, Francielle da Silva and Mataveli, Guilherme
Augusto Verola and Lima, Bruna Sim{\~o}es",
affiliation = "{Universidade Estadual do Oeste do Paran{\'a} (UNIOESTE)} and
{Universidade de S{\~a}o Paulo (USP)} and {Universidade Federal
de S{\~a}o Jo{\~a}o del Rey (UFSJR)} and {Universidade Federal
de S{\~a}o Jo{\~a}o del Rey (UFSJR)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Universidade de S{\~a}o Paulo
(USP)}",
title = "Streamflow and precipitation trends in the Brazilian Amazon basin
and their association with Pacific decadal oscillation and
deforestation",
journal = "Theoretical and Applied Climatology",
year = "2021",
volume = "146",
number = "1/2",
pages = "511--526",
month = "Oct.",
keywords = "Amazon deforestationHydrological cycleSpatial trend analysisPDO
teleconnections.",
abstract = "The Amazon Basin is the region with the highest continental water
density in the world and plays an important role in the global
hydroclimatic system and the carbon cycle. In recent decades, the
Amazon Basin has seen intense land use and land cover change
(LULCC), specifically in terms of the conversion of rainforest
into crop and livestock areas. The feedback mechanisms between the
surface and atmosphere have been modified and biodiversity has
also been endangered. In order to establish the long-term
hydrological trends across the Amazon Basin and possible
relationships with LULCC, monthly data on streamflow and
precipitation obtained from surface stations and remote sensing of
deforestation information from 1976 to 2010 were analyzed.
Homogeneous streamflow sub-regions were determined, and
assessments of these sub-regions show distinct patterns: while the
trend for both rainfall and streamflow is positive in the northern
basin, in the North and Amazon-Mouth sub-regions, the trend is
negative for both variables in the southern basin, the West,
South, and Central sub-regions. In the regions with a negative
trend, the yearly deforestation rate presented high values,
indicating the possible influence of LULCC on the Amazon's
hydrological cycle. Seasonal analysis shows that the reductions in
streamflow and rainfall rates in the southern Amazon Basin were
more frequently registered at the end of the dry season,
indicating a prolonging of this season. Analysis with Global
Precipitation Climatology Centre (GPCC) linear trend data relating
the positive peak of Pacific decadal oscillation (PDO) to the
negative period shows that the negative trend for rainfall and
streamflow in the South sub-region is more intense than the
influence of PDO. This reinforces the hypothesis that
deforestation may be influencing the hydrological cycle in the
Amazon Basin.",
doi = "10.1007/s00704-021-03739-1",
url = "http://dx.doi.org/10.1007/s00704-021-03739-1",
issn = "0177-798X",
language = "en",
targetfile = "Limberger2021_Article_StreamflowAndPrecipitationTren.pdf",
urlaccessdate = "29 jun. 2024"
}