@InProceedings{DallaFaveraMaScCeLuPe:2010:AeOpTh,
author = "Dalla Favera, Alexandre Ceretta and Martins, Fernando Ramos and
Schuch, Nelson Jorge and Ceconi, Marcio and Luiz, Eduardo Weide
and Pereira, Enio Bueno",
affiliation = "{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)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Aerosol optical thickness influence over the Photosynthetically
Active Radiation (PAR) in earth surface - I",
year = "2010",
organization = "The Meeting of the Americas (AGU).",
abstract = "The atmosphere is made up of several components, among them are
present solid and liquid particles in suspension called aerosols.
Aerosols make an important role by absorbing and reflecting
radiation from space. The work aims to evaluate the relationship
between aerosols and Photosynthetically Active Radiation (PAR)
reaching the earth's surface on cloudless-sky days with
development of statistical models. PAR radiation data were
acquired in the SONDA Project network sites located in Campo
Grande - MS, Cuiab{\'a} - MT and Petrolina PE. In addition, data
acquired in Alta Floresta - MT were provided by AERONET. Aerosol
Optical Thickness (AOT) daily average data for all stations were
obtained from the AERONET. The time periods vary according to PAR
and AOT data availability in cloudless-sky days. For Campo Grande,
43 clear sky days in 2008 were analyzed; 116 days from 2006 to
2008 for Cuiab{\'a}; 31 days for the years 2005 and 2007 in
Petrolina; and for Alta Floresta 30 days from 1999 to 2003. Most
of the available data occurs in June, July and August due to dry
season in Brazilian Mid-West and Central regions. Due to the
spectral range of the PAR radiation, 400 nm to 700 nm, AOT data at
wavelengths 675 nm, 500 nm and 440 nm were used in this work.
Linear, polynomial of second degree and exponential empirical
models were developed with 70% of the available data relating the
KPAR parameter and AOT at the specified wavelengths. The KPAR
index is defined as the ratio between the daily PAR irradiation at
the surface and the solar radiation incident on the top of the
atmosphere. The 30% of the remaining data were used to evaluate
model performance. The statistical deviations MBE (Mean Bias
Error) and RMSE (Root Mean Square Error) were used for the models
validation. In general, all models showed satisfactory
performance, as indicated by low statistical deviations. The
polynomial models have presented higher deviations from that of
the others regressions models used. The polynomial models achieve
RMSE values of 11.54% for Alta Floresta in the wavelength of 500
nm, while the exponential and linear models showed, respectively,
2.94 % and 5.78%. The statistical models showed lower deviations
at Campo Grande and Petrolina with an RMSE values around 1.5%. For
the future, it is intend to perform further analysis with larger
data numbers aiming better performance for empirical models, using
also, data from the Reference Station SONDA SMS, installed at the
Southern Space Observatory - SSO/CRS/CCR/INPE - MCT, (29º26' S
53º48' W), for a Brazilian territory extensive investigation.",
conference-location = "Foz do Igua{\c{c}}u",
conference-year = "8-12 Aug. 2010",
language = "en",
targetfile = "01.09.04.11.pdf",
urlaccessdate = "25 abr. 2024"
}