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Aerosol radiometric properties at Western Spain (Cáceres station)
Author(s) -
Obregón M. A.,
Serrano A.,
Cancillo M. L.,
Cachorro V. E.,
Toledano C.
Publication year - 2015
Publication title -
international journal of climatology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.58
H-Index - 166
eISSN - 1097-0088
pISSN - 0899-8418
DOI - 10.1002/joc.4031
Subject(s) - aerosol , aeronet , environmental science , sun photometer , single scattering albedo , atmospheric sciences , albedo (alchemy) , turbidity , climatology , angstrom exponent , optical depth , meteorology , geology , oceanography , geography , art , performance art , art history
ABSTRACT This paper analyses the radiometric properties of aerosol column over Western Spain. It is based on 7‐year data series of aerosol parameters at the AERONET Cáceres station (Spain) as measured by CIMEL sun‐photometers. The study period extends along almost 7 years: from July 2005 to June 2012. The paper aims at analysing the temporal evolution, mean values and spectral dependence of some fundamental aerosol parameters such as aerosol optical depth ( τ ), Ångström parameter ( α ), single scattering albedo (ω), asymmetry parameter ( g ) and volume size distribution ( dV dlogr −1 ); and their relationship with the most frequent air masses that arrive at Western Spain. Mean values correspond to aerosols of small size and low concentration (mean τ 500 = 0.11; mean α = 1.38). In fact, 50% of days correspond to ‘continental‐clean’ type. However, there is a certain variability of conditions, with more than 25% of medium and high turbidity cases with τ 500 higher than 0.20. These episodes of high turbidity occur more frequently in August and September and are usually due to the influence of desert‐dust aerosol, biomass burning, continental aerosol, or a mixture of them. The analysis of the all basic and derived aerosol parameters is explained by the main influences: continental location, exposed to maritime aerosols coming from the Atlantic Ocean, and affected by Saharan dust intrusions.