Sorooshian A, Shingler T, Harpold A, Feagles C W, Meixner T, Brooks P D
Department of Chemical and Environmental Engineering, University of Arizona, Tucson, Arizona, USA ; Department of Atmospheric Sciences, University of Arizona, Tucson, Arizona, USA.
Department of Chemical and Environmental Engineering, University of Arizona, Tucson, Arizona, USA.
Atmos Chem Phys. 2013 Aug 1;13(15):7361-7379. doi: 10.5194/acp-13-7361-2013.
This study characterizes the spatial and temporal patterns of aerosol and precipitation composition at six sites across the United States Southwest between 1995 and 2010. Precipitation accumulation occurs mostly during the wintertime (December-February) and during the monsoon season (July-September). Rain and snow pH levels are usually between 5-6, with crustal-derived species playing a major role in acid neutralization. These species (Ca, Mg, K, Na) exhibit their highest concentrations between March and June in both PM and precipitation due mostly to dust. Crustal-derived species concentrations in precipitation exhibit positive relationships with [Formula: see text], [Formula: see text], and Cl, suggesting that acidic gases likely react with and partition to either crustal particles or hydrometeors enriched with crustal constituents. Concentrations of particulate [Formula: see text] show a statistically significant correlation with rain [Formula: see text] unlike snow [Formula: see text], which may be related to some combination of the vertical distribution of [Formula: see text] (and precursors) and the varying degree to which [Formula: see text]-enriched particles act as cloud condensation nuclei versus ice nuclei in the region. The coarse : fine aerosol mass ratio was correlated with crustal species concentrations in snow unlike rain, suggestive of a preferential role of coarse particles (mainly dust) as ice nuclei in the region. Precipitation [Formula: see text] : [Formula: see text] ratios exhibit the following features with potential explanations discussed: (i) they are higher in precipitation as compared to PM; (ii) they exhibit the opposite annual cycle compared to particulate [Formula: see text] : [Formula: see text] ratios; and (iii) they are higher in snow relative to rain during the wintertime. Long-term trend analysis for the monsoon season shows that the [Formula: see text] : [Formula: see text] ratio in rain increased at the majority of sites due mostly to air pollution regulations of [Formula: see text] precursors.
本研究描绘了1995年至2010年间美国西南部六个地点气溶胶和降水成分的时空模式。降水主要集中在冬季(12月至2月)和季风季节(7月至9月)。雨雪的pH值通常在5至6之间,地壳来源的物质在酸中和中起主要作用。这些物质(钙、镁、钾、钠)在3月至6月期间在颗粒物和降水中浓度最高,主要是由于沙尘。降水中地壳来源物质的浓度与[公式:见正文]、[公式:见正文]和氯呈正相关,表明酸性气体可能与富含地壳成分的地壳颗粒或水凝物发生反应并分配到其中。颗粒物[公式:见正文]的浓度与雨水中的[公式:见正文]呈统计学显著相关,与雪水中的[公式:见正文]不同,这可能与[公式:见正文](及其前体)的垂直分布以及富含[公式:见正文]的颗粒在该地区作为云凝结核与冰核的不同程度的某种组合有关。与雨不同,粗颗粒物与细颗粒物的质量比与雪中地壳物质的浓度相关,这表明粗颗粒物(主要是沙尘)在该地区作为冰核具有优先作用。降水[公式:见正文] : [公式:见正文]比值呈现出以下特征,并对其潜在解释进行了讨论:(i)与颗粒物相比,降水中的该比值更高;(ii)与颗粒物[公式:见正文] : [公式:见正文]比值相比,其呈现相反的年周期;(iii)在冬季,雪中的该比值相对于雨水中的更高。对季风季节的长期趋势分析表明,大多数地点雨水中的[公式:见正文] : [公式:见正文]比值增加,主要是由于[公式:见正文]前体的空气污染法规。