@Article{AlcāntaraBoAsStNoLo:2010:InReIt,
author = "Alc{\^a}ntara, Enner Herenio de and Bonnet, M. P. and Assireu,
Arcilan Trevenzoli and Stech, Jos{\'e} Luis and Novo, Evlyn
M{\'a}rcia Le{\~a}o de Moraes and Lorenzzetti, Jo{\~a}o
Antonio",
affiliation = "{} and {} and {Instituto Nacional de Pesquisas Espaciais (INPE)}
and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "On the water thermal response to the passage of cold fronts:
initial results for Itumbiara reservoir (Brazil)",
journal = "Hydrology and Earth System Sciences Discussions",
year = "2010",
volume = "7",
pages = "9437--9465",
note = "{Setores de Atividade: Educa{\c{c}}{\~a}o.}",
keywords = "Limnologia, Frentes Frias, Reservat{\'o}rios, Fluxos de calor.",
abstract = "The passage of meteorological systems such as cold fronts or
convergence zones over reservoirs can cause significant
modifications in several aquatic variables. Cold fronts coming
from higher latitudes and reaching the Southeastern Brazilian
territory modify the mean wind field and have important impact
over physical, chemical and biological processes that act in the
hydroelectric reservoirs. The mean period of cold front passages
along the Southeastern Brazilian coast is 6 days during the winter
and between 11 and 14 days in the summer. Most of these fronts
also affect the hinterland of S{\~a}o Paulo, Minas Gerais and
Goi{\'a}s states. The objective of this work is to analyze the
influence of cold front passages in the thermal stratification and
water quality of the Itumbiara hydroelectric reservoir which is
located in Minas Gerais and Goi{\'a}s. The characterization of
cold front passages over the study area was done through the
analysis of GOES satellite images. The analyzed data set includes
time series of meteorological (wind direction and intensity,
short-wave radiation, air temperature, relative humidity,
atmospheric pressure) and water temperature in four depths (5, 12,
20 and 40 m). The data set was acquired in the interior of the
reservoir by an autonomous anchored buoy system at a sampling rate
of 1 h. The stratification was assessed by non-dimensional
parameter analysis. The lake number an indicator of the degree of
stability and mixing in the reservoir was used in this analysis.
We will show that during the cold front all atmospheric parameters
respond and this response are transferred immediately to the water
surface. The main effect is observed in the water column, when the
heat loss in the surface allows the upwelling events caused by
convective cooling due to the erosion of thermal stratification.",
doi = "10.5194/hessd-7-9437-2010",
url = "http://dx.doi.org/10.5194/hessd-7-9437-2010",
issn = "1812-2108",
label = "lattes: 3852581196429739 6 Alc{\^a}ntaraBoAsStNoLo:2010:InReIt",
language = "en",
targetfile = "hessd-7-9437-2010-print.pdf",
urlaccessdate = "03 maio 2024"
}