Influence of air mass origins on optical properties and PM concentrations measured at a high mountain station located in the southwestern Mediterranean

摘要

The influence of air mass origins on aerosol optical properties and particulate matter (PM) concentrations measured from January 2014 to December 2015 at a high mountain station in the southwestern Mediterranean was analyzed. Mean values of extensive aerosol optical properties (scattering, backscattering and absorption coefficients) and PM mass fractions: sigma(sp) (30.7 +/- 1.1 Mm(-1)), sigma(bsp) (3.9 +/- 0.1 Mm(-1)), sigma(ap) (2.4 +/- 0.1 Mm(-1)), PM10 (13.1 +/- 0.6 mu.gm(-3)) and PM1 (4.0 +/- 0.1 mu.gm(-3)) were in the range of values reported in most studies carried out at high altitude locations. Nevertheless, a significant variation of these concentrations according to the air mass origin has been noticed. Transport from North Africa (NAF back -trajectories) and regional re circulations (REG) were the two air mass types in which the highest values of PM concentrations and optical properties were registered. Alternatively, the lowest values were recorded under Atlantic advections. Noticeable differences between NAF and REG categories were observed when intensive optical properties of aerosols were analyzed. During NAF scenarios the lowest value of SAE (0.91 +/- 0.06) was obtained as well as the greatest AAE value (1.30 +/- 0.02), with daily levels higher than 1.90. This result suggests that OC and hematite compounds were relevant in the absorption process during NAF events. However, during REG episodes the AAE mean value declined to 1.18 +/- 0.01, since the highest mean concentration of BC was recorded under this category, and the SAE value was maximum (1.70 +/- 0.05) due to the smaller size of PM. It has also been documented that during the study period a great number of REG back-trajectories occurred just after the transport of air masses from North Africa. In these situations, AAE and SAE values showed slight variations due to the persistence of mineral dust in the local atmosphere.