@Article{AimiZBSHRRDMVBHR:2021:EvAtDo,
author = "Aimi, Daniele and Zimmer, Tamires and Buligon, Lidiane and Souza,
Vanessa de Arruda and Hernandez, Roilan and Romio, Leugim Corteze
and Rubert, Gisele Cristina Dotto and Diaz, Marcelo Bortoluzzi and
Maldaner, Silvana and Veeck, Gustavo Pujol and Bremm, Tiago and
Herdies, Dirceu Luis and Roberti, Debora Regina",
affiliation = "{Universidade Federal de Santa Maria (UFSM)} and {Universidade
Federal de Santa Maria (UFSM)} and {Universidade Federal de Santa
Maria (UFSM)} and {Universidade Federal de Santa Maria (UFSM)} and
{Universidade Federal de Santa Maria (UFSM)} and {Universidade
Federal do Pampa (UNIPAMPA)} and {Universidade Federal de Santa
Maria (UFSM)} and {Universidade Federal de Santa Maria (UFSM)} and
{Universidade Federal de Santa Maria (UFSM)} and {Universidade
Federal de Santa Maria (UFSM)} and {Universidade Federal de Santa
Maria (UFSM)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Universidade Federal de Santa Maria (UFSM)}",
title = "Evaluation of atmospheric downward longwave radiation in the
brazilian pampa region",
journal = "Atmosphere",
year = "2021",
volume = "12",
number = "1",
pages = "1--17",
month = "Jan.",
keywords = "atmospheric downward longwave radiation, Pampa biome, statistical
analyses, modeling.",
abstract = "Atmospheric downward longwave radiation flux (L\↓) is a
variable that directly influences the surface net radiation and
consequently, weather and climatic conditions. Measurements of
L\↓ are scarce, and the use of classical models depending
on some atmospheric variables may be an alternative. In this
paper, we analyzed L\↓ measured over the Brazilian Pampa
biome. This region is located in a humid subtropical climate zone
and characterized by well defined seasons and well distributed
precipitation. Furthermore, we evaluated the performance of the
eleven classical L\↓ models for clear sky with one-year
experimental data collected in the Santa Maria experimental site
(SMA) over native vegetation and high relative humidity throughout
the year. Most of the L\↓ estimations, using the original
coefficients, underestimated the experimental data. We performed
the local calibration of the L\↓ equations coefficients
over an annual period and separated them into different sky cover
classifications: clear sky, partly cloudy sky, and cloudy sky. The
calibrations decreased the errors, especially in cloudy sky
classification. We also proposed the joint calibration between the
clear sky emissivity equations and cloud sky correction function
to reduce errors and evaluate different sky classifications. The
results found after these calibrations presented better
statistical indexes. Additionally, we presented a new empirical
model to estimate L\↓ based on multiple regression analysis
using water vapor pressure and air temperature. The new equation
well represents partial and cloudy sky, even without including the
cloud cover parameterization, and was validated with the following
five years in SMA and two years in the Cachoeira do Sul
experimental site (CAS). The new equation proposed herein presents
a root mean square error ranging from 13 to 21 Wm\−2 and
correlation coefficient from 0.68 to 0.83 for different sky cover
classifications. Therefore, we recommend using the novel equation
to calculate L\↓ over the Pampa biome under these specific
climatic conditions.",
doi = "10.3390/atmos12010028",
url = "http://dx.doi.org/10.3390/atmos12010028",
issn = "2073-4433",
language = "en",
targetfile = "aimi_evaluation.pdf",
urlaccessdate = "20 maio 2024"
}