title: Aerosol and precipitation chemistry in the southwestern United States: spatiotemporal trends and interrelationships.
abstract: 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 (Ca2+, Mg2+, K+, Na+) exhibit their highest concentrations between March and June in both PM2.5and 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 PM2.5; (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.
authors.affiliation: Department of Chemical and Environmental Engineering, University of Arizona, Tucson, Arizona, USA ; Department of Atmospheric Sciences, University of Arizona, Tucson, Arizona, USA.
authors.forename: A
authors.initials: A
authors.lastname: Sorooshian
authors.affiliation: Department of Chemical and Environmental Engineering, University of Arizona, Tucson, Arizona, USA.
authors.forename: T
authors.initials: T
authors.lastname: Shingler
authors.affiliation: Department of Hydrology and Water Resources, University of Arizona, Tucson, Arizona, USA ; Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, Colorado, USA.
authors.forename: A
authors.initials: A
authors.lastname: Harpold
authors.affiliation: Department of Chemical and Environmental Engineering, University of Arizona, Tucson, Arizona, USA.
authors.forename: C W
authors.initials: CW
authors.lastname: Feagles
authors.affiliation: Department of Hydrology and Water Resources, University of Arizona, Tucson, Arizona, USA.
authors.forename: T
authors.initials: T
authors.lastname: Meixner
authors.affiliation: Department of Hydrology and Water Resources, University of Arizona, Tucson, Arizona, USA.
authors.forename: P D
authors.initials: PD
authors.lastname: Brooks