Inmaculada Foyo Moreno

Dr. Inmaculada Foyo Moreno

orcid

Research Focus & Metrics

Academic Career Length

37Years (1990-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 January 1996 in Agricultural and Forest Meteorology
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Journal Article
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IAI. Alados
I. Alados
IMInmaculada Foyo Moreno
Inmaculada Foyo Moreno
Lucas Alados-ArboledasLucas Alados-Arboledas
Lucas Alados-Arboledas

22 February 2012 in Journal of Geophysical Research: Atmospheres
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Gloria TitosGloria Titos
Gloria Titos
IMInmaculada Foyo Moreno
Inmaculada Foyo Moreno
HLHassan Lyamani
Hassan Lyamani
XQXavier Querol
Xavier Querol
Andrés Alastuey UrósAndrés Alastuey Urós
Andrés Alastuey Urós
Lucas Alados-ArboledasLucas Alados-Arboledas
Lucas Alados-Arboledas
We investigated aerosol optical properties, mass concentration and chemical composition over a 1 year period (from March 2006 to February 2007) at an urban site in Southern Spain (Granada, 37.18°N, 3.58°W, 680 m above sea level). Light‐scattering and absorption measurements were performed using an integrating nephelometer and a MultiAngle Absorption Photometer (MAAP), respectively, with no aerosol size cut‐off and without any conditioning of the sampled air. PM10 and PM1 (ambient air levels of atmospheric particulate matter finer than 10 and 1 microns) were collected with two high volume samplers, and the chemical composition was investigated for all samples. Relative humidity (RH) within the nephelometer was below 50% and the weighting of the filters was also at RH of 50%. PM10 and PM1 mass concentrations showed a mean value of 44 ± 19 μg/m3 and 15 ± 7 μg/m3, respectively. The mineral matter was the major constituent of the PM10–1 fraction (contributing more than 58%) whereas organic matter and elemental carbon (OM+EC) contributed the most to the PM1 fraction (around 43%). The absorption coefficient at 550 nm showed a mean value of 24 ± 9 Mm−1 and the scattering coefficient at 550 nm presented a mean value of 61 ± 25 Mm−1, typical of urban areas. Both the scattering and the absorption coefficients exhibited the highest values during winter and the lowest during summer, due to the increase in the anthropogenic contribution and the lower development of the convective mixing layer during winter. A very low mean value of the single scattering albedo of 0.71 ± 0.07 at 550 nm was calculated, suggesting that urban aerosols in this site contain a large fraction of absorbing material. Mass scattering and absorption efficiencies of PM10 particles exhibited larger values during winter and lower during summer, showing a similar trend to PM1 and opposite to PM10–1. This seasonality is therefore influenced by the variations on PM composition. In addition, the mass scattering efficiency of the major aerosol constituents in PM10 were also calculated applying the multilinear regression (MLR) analysis. Among all of them, the most efficient in terms of scattering was sulfate ion (7 ± 1 m2g−1) while the least efficient was the mineral matter (0.2 ± 0.3 m2g−1). On the other hand, we found that the absorption process was mainly dominated by carbonaceous particles.

1 December 2003 in Agricultural and Forest Meteorology
Verified
Journal Article
Closed access
IMInmaculada Foyo Moreno
Inmaculada Foyo Moreno
IAI. Alados
I. Alados
FOF.J. Olmo
F.J. Olmo
Lucas Alados-ArboledasLucas Alados-Arboledas
Lucas Alados-Arboledas

1 July 1999 in Journal of Applied Meteorology and Climatology
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Journal Article
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IMInmaculada Foyo Moreno
Inmaculada Foyo Moreno
Jerónimo Vida ManzanoJerónimo Vida Manzano
Jerónimo Vida Manzano
Lucas Alados-ArboledasLucas Alados-Arboledas
Lucas Alados-Arboledas
A new expression to estimate the solar ultraviolet irradiance from parameters usually available in radiometric networks is presented. The authors have analyzed the relation between solar ultraviolet global irradiance (290–385 nm), UV, and broadband global irradiance, G, studying as well the ratio UV/G. The analysis of the dependence between the ultraviolet global irradiance and the broadband global irradiance, both normalized to their respective extraterrestrial values, has been used in order to develop a functional dependence between both global hemispherical transmittances. The cloud radiative effect on both radiometric fluxes has also been studied. After this analysis, the authors propose a new expression to obtain ultraviolet global irradiance from only two input variables: clear-sky ultraviolet irradiance and the global broadband hemispherical transmittance. The dataset used in this paper has been registered in two-radiometric stations: one located in the outskirts of Granada (37.18°N, 3.58°... Abstract A new expression to estimate the solar ultraviolet irradiance from parameters usually available in radiometric networks is presented. The authors have analyzed the relation between solar ultraviolet global irradiance (290–385 nm), UV, and broadband global irradiance, G, studying as well the ratio UV/G. The analysis of the dependence between the ultraviolet global irradiance and the broadband global irradiance, both normalized to their respective extraterrestrial values, has been used in order to develop a functional dependence between both global hemispherical transmittances. The cloud radiative effect on both radiometric fluxes has also been studied. After this analysis, the authors propose a new expression to obtain ultraviolet global irradiance from only two input variables: clear-sky ultraviolet irradiance and the global broadband hemispherical transmittance. The dataset used in this paper has been registered in two-radiometric stations: one located in the outskirts of Granada (37.18°N, 3.58°...

1 May 2003 in Agricultural and Forest Meteorology
Verified
Journal Article
Closed access
IAI Alados
I Alados
IMInmaculada Foyo Moreno
Inmaculada Foyo Moreno
FOF.J Olmo
F.J Olmo
Lucas Alados-ArboledasLucas Alados-Arboledas
Lucas Alados-Arboledas

1 May 2003 in Atmospheric Research
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Journal Article
Closed access
Lucas Alados-ArboledasLucas Alados-Arboledas
Lucas Alados-Arboledas
IAI. Alados
I. Alados
IMInmaculada Foyo Moreno
Inmaculada Foyo Moreno
FOF.J. Olmo
F.J. Olmo
AAA. Alcántara
A. Alcántara