@Article{Luiz-SilvaMaceRotuChou:2022:PrFuHy,
author = "Luiz-Silva, Wanderson and Maceira, Maria Elvira Piņero and Rotunno
Filho, Otto Corr{\^e}a and Chou, Sin Chan",
affiliation = "{Centro de Pesquisa em Energia El{\'e}trica (CEPEL)} and {Centro
de Pesquisa em Energia El{\'e}trica (CEPEL)} and {Universidade
Federal do Rio de Janeiro (UFRJ)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "On the observations and environmental modeling in Xing{\'o}
Hydropower Plant - northeast Brazil: present and future
hydroclimatic features",
journal = "Environmental Modeling and Assessment",
year = "2022",
volume = "27",
number = "1",
pages = "13--28",
month = "Feb.",
keywords = "Climate change, Climate model, Hydropower, Precipitation,
Streamflow, S{\~a}o Francisco.",
abstract = "The S{\~a}o Francisco River Basin plays a critical role in the
hydroelectrical operational planning of Brazil. Understanding the
hydroclimatic dynamic regime and, consequently, related climate
changes is essential for decision-makers of the hydroelectrical
sector. In this context, the Xing{\'o} hydropower plant and its
drainage area are taken as a reference for the hydroclimatic
features analyzed in this research. Observed rainfall in the
drainage basin and streamflow measurements in the power plant
between 1975 and 2016 are used to assess the climatology of the
region and to identify trends in the time series. In addition, a
methodological framework based on numerical modeling of the
hydroclimatic variables is employed to examine the representation
of the present climate (1961 to 1990) and to investigate the
future projections (2011 to 2100). The outputs from the Eta
regional climate model runs driven by two global models are
adopted in this case under the RCP4.5 and RCP8.5 IPCC scenarios
along with the SMAP rainfall-runoff model. In Xing{\'o}, the
average annual precipitation is about 978 mm and the average
annual streamflow is 2,534 m3 s\−1. The size of the
Xing{\'o} HPP drainage area must be considered, as the rainfall
that occurs in a given month can influence the streamflow of the
following month. There is no trend regarding precipitation, while
the streamflow time series show a statistically significant
decreasing trend in the present climate. Climate projections point
to an elevation in air temperature and a reduction in rainfall and
streamflow by 2100. Most scenarios indicate that the average
annual streamflow could be extremely low for nearly half of the
twenty-first century. The results shown in this work may
contribute to scenarios for operation of the Xing{\'o} HPP and
support with information for planning decisions on country's
energy security in the present and future climates.",
doi = "10.1007/s10666-021-09810-5",
url = "http://dx.doi.org/10.1007/s10666-021-09810-5",
issn = "1420-2026",
language = "en",
targetfile = "Luiz-Silva2022_Article_OnTheObservationsAndEnvironmen.pdf",
urlaccessdate = "25 jun. 2024"
}