@Article{AssireuAlNoRoPaStLo:2011:AnSaIn,
author = "Assireu, Arcilan Trevenzoli and Alc{\^a}ntara, Enner Herenio and
Novo, Evlyn M{\'a}rcia Le{\~a}o de Moraes and Roland, Fabio and
Pacheco, Felipe Siqueira and Stech, Jos{\'e} Luis and
Lorenzzetti, Jo{\~a}o Antonio",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and Aquatic
Ecology Laboratory, Biological Science Institute, Federal
University of Juiz de Fora, MG, Brazil and Aquatic Ecology
Laboratory, Biological Science Institute, Federal University of
Juiz de Fora, MG, Brazil and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)}",
title = "Inside the hydro-physics processes at the plunge point location:
an analysis by satellite and in situ data",
journal = "Hydrology and Earth System Sciences Discussions",
year = "2011",
volume = "8",
pages = "1193--1223",
month = "Jan.",
abstract = "The plunge point locates the main point of mixing between river
and the epilimnion reservoir water. The plunge point monitoring is
essential to understand how it will be the behavior of density
currents and its implications for reservoir. The applicability of
satellite imagery products from different sensors (Landsat TM band
6 thermal signatures and visible channel) for characterization of
the river-reservoir transition zone is presented in this study. We
demonstrate the feasibility of the Landsat TM band imagery to
discern the subsurface river plumes and the plunge point. The
spatial variability of the plunge point evident in the hydrologic
data illustrates the advantages of synoptic satellite measurements
over in situ point measurements alone to detect the
river-reservoir transition zone. It is indicated that the river
flowing as underflow contributes to the thermal stability of the
water column during wet season (summer-autumn). During the dry
season, when the river-reservoir water temperature differences
vanish and the river circulation is characterized by
interflow-overflow, the river water inserts into the reservoir
upper layers, affecting water quality. The results indicate good
agreement between hydrologic and satellite data and that the
jointly use of thermal and visible channel, operational monitoring
of plunge point is feasible. The deduced information about the
density current from this product could potentially be assimilated
for numerical modeling and hence be of significant interest for
environmental and climatological research.",
doi = "10.5194/hessd-8-1193-2011",
url = "http://dx.doi.org/10.5194/hessd-8-1193-2011",
issn = "1812-2108",
label = "lattes: 9857505876280820 3 AssireuAlNoRoPaStLo:2011:AnSaIn",
language = "en",
targetfile = "hessd-8-1193-2011assireu.pdf",
urlaccessdate = "16 jun. 2024"
}