@Article{CurtarelliAlcāRennStec:2013:EfCoFr,
author = "Curtarelli, Marcelo Pedroso and Alc{\^a}ntara, Enner and
Renn{\'o}, Camilo and Stech, Jos{\'e} Luiz",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and Department
of Cartography, S{\~a}o Paulo State University, Presidente
Prudente, SP, Brazil and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)}",
title = "Effects of cold fronts on MODIS-derived sensible and latent heat
fluxes in Itumbiara reservoir (Central Brazil)",
journal = "Advances in Space Research",
year = "2013",
volume = "52",
number = "9",
pages = "1668--1677",
month = "Nov.",
keywords = "cold front, hydroelectric reservoirs, MODIS, sensible and latent
heat fluxes, sensible heat flux, tropical reservoirs, unstable
conditions, water surface temperature, atmospheric temperature,
heat flux, heat losses, radiometers, water content, reservoirs
(water).",
abstract = "In this work we investigate the cold front passage effects on
sensible and latent heat flux in a tropical hydroelectric
reservoir. The study area, Itumbiara reservoir (Goi{\'a}s
State/Brazil) at the beginning of the austral winter, is
characterized by the presence of a weak thermal stratification and
the passage of several cold fronts from higher latitudes of South
America. Sensible and latent heat fluxes were estimated
considering the atmospheric boundary layer stability. In situ and
MODIS water surface temperature data were used to adjust the
coefficients for momentum and heat exchanges between water and
atmosphere and spatialize the sensible and latent heat fluxes. The
results showed that during a cold front event the sensible heat
flux can be up to five times greater than the flux observed
before. The latent heat flux tends to decrease during the cold
front but increase again after the passage. The highest values of
heat loss were observed at littoral zone and some Reservoir's
embayment. The heat loss intensification can be separated in two
moments: first, during the cold front passage, when the wind speed
increases and the air temperature decreases; second, after the
cold front passage, with air humidity decreasing. This can be
considered a key process to understanding the heat loss in the
Itumbiara reservoir.",
doi = "10.1016/j.asr.2013.07.037",
url = "http://dx.doi.org/10.1016/j.asr.2013.07.037",
issn = "0273-1177",
label = "scopus 2013-11",
language = "en",
targetfile = "1-s2.0-S0273117713004663-main.pdf",
urlaccessdate = "03 maio 2024"
}