2017
DOI: 10.1016/j.atmosres.2017.07.013
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Influence of air mass origins on optical properties and PM concentrations measured at a high mountain station located in the southwestern Mediterranean

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Cited by 12 publications
(11 citation statements)
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“…This implies that ~26% of the days of the year were under the influence of SDE. This percentage is consistent with those obtained by Galindo et al (2017) and Castañer et al (2017) at a high mountain station (> 1500 m a.s.l.) located approximately 200 km southeast.…”
Section: Characterization Of Sdesupporting
confidence: 91%
“…This implies that ~26% of the days of the year were under the influence of SDE. This percentage is consistent with those obtained by Galindo et al (2017) and Castañer et al (2017) at a high mountain station (> 1500 m a.s.l.) located approximately 200 km southeast.…”
Section: Characterization Of Sdesupporting
confidence: 91%
“…Table 2). The effects of long-transported air parcels on the aerosol particles and its composition and sources have been discussed in previous studies [82][83][84][85] . The Asian dust particles blow from these areas in the westerly wind and play an important role in the leeward ecosystem.…”
Section: Inhalable Bacterial Community In Pm 25mentioning
confidence: 99%
“…This value was higher than that recorded in the absence of events (0.776). Values close to or above 0.900 (λ = 520 nm) have been previously obtained in the Iberian Peninsula during Saharan events [17,[39][40][41]. The spectral variation of SSA can provide useful information about the dominance of specific aerosol types (e.g., BC, organic carbon, dust, sulfates) during events [42,43].…”
Section: Aop Variations As a Function Of The Characteristics Of Sdementioning
confidence: 64%
“…Aerosol optical properties (AOP) can undergo significant variations under the influence of SDE. Several studies carried out in the Iberian Peninsula have analyzed the impact of SDE on AOP [12][13][14][15][16][17]. The main variations in AOP during SDE include: increases in the scattering (σ sp ) and absorption (σ ap ) coefficients; a rise in the Absorption Angström Exponent (AAE) due to the absorption of UV and visible radiation by MD; a drop in the Scattering Angström Exponent (SAE) because of the predominance of coarse particles during these events; and a rise in the Single Scattering Albedo (SSA) value since the relative increase in σ sp is greater than that in σ ap .…”
Section: Introductionmentioning
confidence: 99%