@InProceedings{AlcântaraStCaBoLoNo:2010:SpWaTe,
author = "Alc{\^a}ntara, Enner Herenio de and Stech, Jos{\'e} and
Casamitjana, Xavier and Bonnet, Marie Paule and Lorenzzetti,
Jo{\~a}o A. and Novo, Evlyn",
affiliation = "undefined and {} and {} and {} and undefined and undefined",
title = "On the spatially water temperature and heat flux variability over
a tropical hydroelectric reservoir",
booktitle = "Proceedings...",
year = "2010",
editor = "Andrad{\'o}ttir, Hrund {\'O}l{\"o}f",
pages = "8--15",
organization = "International Workshop on Physical Processes in Natural Waters,
14.",
publisher = "University of Iceland",
address = "Iceland",
keywords = "Remote sensing, water surface temperature, heat flux, mixed depth
layer, thermal amplitude, MODIS.",
abstract = "Water temperature plays an important role in ecological
functioning and in controlling the biogeochemical processes of a
water body. Conventional water quality monitoring is expensive and
time consuming. It is particularly problematic if the water bodies
to be examined are large. Conventional techniques also bring about
a high probability of undersampling. Conversely, remote sensing is
a powerful tool to assess aquatic systems. The objective of this
study was to map the surface water temperature and improve
understanding of spatiotemporal variations in a hydroelectric
reservoir. In this work, MODIS land-surface temperature (LST)
level 2, 1-km nominal resolution data (MOD11L2, version 5) were
used. All available clear-sky MODIS/Terra images from 2003 to 2008
were used, resulting in a total of 786 daytime and 473 nighttime
images. Descriptive statistics (mean, maximum and minimum) were
computed for the historical images to build a time series of
daytime and nighttime monthly mean temperatures. The thermal
amplitude and anomaly were also computed. In-situ meteorological
variables were used from 2003 to 2008 to help understand the
spatiotemporal variability of the surface water temperature. The
surface energy budget and the depth at which the wind can
distribute the heat input of a given surface were also measured. A
correlation between daytime and nighttime surface water
temperatures and the computed heat fluxes were made. These
relationships and the causes of the water surface temperature
variability are discussed.",
conference-location = "Reykjav{\'{\i}}k Reykjav{\'{\i}}k",
conference-year = "June 28 - July 1, 2010",
isbn = "978-9979-9812-9-9",
label = "lattes: 7939379291404418 1 Alc{\^a}ntaraStCaBoLoNo:2010:SpWaTe",
language = "en",
targetfile = "alcantara1.pdf",
url = "http://vefsetur.hi.is/ppnw/en/about_ppnw_workshop_1",
urlaccessdate = "05 maio 2024"
}