@Article{SantosCarBorGasBor:2021:IsCoPr,
author = "Santos, Cleber Assis dos and Carneiro, Rayonil and Borges, Camilla
and Gastmans, Didier and Borma, Laura de Simone",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Universidade Federal
de Campina Grande (UFCG)} and {Universidade Estadual Paulista
(UNESP)} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Isotopic composition of precipitation in a southeastern region of
Brazil during the action of the south Atlantic convergence zone",
journal = "Atmosphere",
year = "2021",
volume = "12",
number = "4",
pages = "e418",
month = "Apr.",
keywords = "moisture of Amazon, stable isotopes \δ,,, 2H and \δ,,,
18O, tropical region, precipitation, Brazil.",
abstract = "The use of stable isotopes of hydrogen and oxygen is a tool widely
used to trace water paths along the hydrological cycle, providing
support for understanding climatic conditions in different spatial
scales. One of the main synoptic scale events acting in
southeastern Brazil is the South Atlantic Convergence Zone (SACZ),
which causes a large amount of precipitation from southern
Amazonia to southeastern Brazil during the southern summer. In
order to determine the isotopic composition of precipitation
during the action of SACZ in S{\~a}o Francisco Xavier in
southeastern Brazil, information from the Weather Forecasting and
Climate Studies Center of the National Institute for Space
Research (CPTEC) was used regarding SACZ performance days, the
retrograde trajectories of the HYSPLIT model, and images from the
GOES-16 satellite, in addition to the non-parametric statistical
tests by Spearman and Kruskal-Wallis. A high frequency of air mass
trajectories from the Amazon to southeastern Brazil was observed
when the SACZ was operating. During the SACZ events, the average
isotopic composition of precipitation was more depleted, with a
\δ18O of \−9.9 (±2.1), a \δ2H of \−69.3
(±17.9), and d-excess of 10.1 (±4.0). When disregarding the SACZ
performance, the annual isotopic composition can present an
enrichment of 1.0 for \δ18O and 8.8 for the \δ2H. The
long-term monitoring of trends in the isotopic composition of
precipitation during the SACZ events can assist in indicating the
evapotranspiration contribution of the Amazon rainforest to the
water supply of southeastern Brazil.",
doi = "10.3390/atmos12040418",
url = "http://dx.doi.org/10.3390/atmos12040418",
issn = "2073-4433",
language = "en",
targetfile = "santos_isotopic.pdf",
urlaccessdate = "07 maio 2024"
}