@Article{LemesOliFisTedSil:2020:AnMoTr,
author = "Lemes, Murilo da Costa Ruv and Oliveira, Gilvan Sampaio de and
Fisch, Gilberto and Tedeschi, Renata Gon{\c{c}}alves and Silva,
Jo{\~a}o Pedro Rodrigues da",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Universidade de
Taubat{\'e} (UNITAU)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Universidade de S{\~a}o Paulo (USP)}",
title = "Analysis of Moisture Transport from Amazonia to Southeastern
Brazil During the Austral Summer",
journal = "Revista Brasileira de Geografia F{\'{\i}}sica",
year = "2020",
volume = "13",
number = "6",
pages = "2650--2670",
keywords = "ENSO Brazil, Climate Change, GPCP, reanalysis.",
abstract = "In two recent Austral summers (between the years 2013/14 and
2014/15), a southeastern region of Brazil suffered a period of
severe drought. The main convective activity during the summer
(mainly responsible for the rain) is an interconnected band of
cloudiness with NW / SE orientation, which extends from the
adjacent Atlantic Ocean to the SW of the Amazon, being called the
South Atlantic Convergence Zone (SACZ). In addition to the SACZ,
the passage of frontal systems also affects the rainfall
distribution as well as some moisture oceanic input from the
Atlantic Subtropical High pressure. Thus, the main objective of
this work is to compute the moisture transfer from the Amazon
region to the south and southeast of Brazil and associate it with
the precipitation pattern. In addition, the influence of different
types of El Niņo Southern Oscillation (ENSO) in the moisture flow,
for instance, Central (higher temperatures in the central
equatorial Pacific) and East (higher temperatures in the eastern
equatorial Pacific) were also studied. The summer of 2013/14 was
the driest of the series (1979 - 2016). Although it was below the
climatology, the precipitation trend found for the period is not
significant, according Mann-Kendall test. However, it is clearly
notable the importance of the moisture transport from the Amazon
region to the southeast in neutral years, providing huge
accumulated rainfall. Moreover, it is possible to affirm that
there is a such significant difference in the intensity of the
moisture flow in neutral years. Although, this intensity can be
influenced by the position of the greatest anomaly of the sea
surface temperature (ASST) in the Pacific. In other words, if this
anomaly is greater in the eastern portion of the ocean (named as
East El Niņo Leste) an intensification in the flow is identified
which will produce a greater amount of moisture in the regions.
However, if the ASST is greater in the central region (El Niņo
Central), this intensification is lower, which may result in
changes in the volume of precipitation in the region.",
issn = "1984-2295",
language = "en",
targetfile = "lemes_analysis.pdf",
urlaccessdate = "19 abr. 2024"
}