Traditional particulate matter (PM) studies focus on atmospheric transport and source identification. Focusing on a problematic airshed in southwestern North America, we analyzed atmospheric characteristics and hydroclimatic conditions leading to high concentrations of PM most representative of dust (PM 10 ). The bi-national airshed of Nogales (Arizona, USA and Sonora, Mexico), has been historically characterized by high PM 10 concentrations, which tend to be much higher on the Sonora side. Concentrations in greater Nogales tend to be highest in fall and winter and lowest in summer, despite climatologically moister soil conditions in fall and winter. Within the fall, winter, and spring seasons, days of high and low PM 10 concentration were primarily distinguished by the condition of the atmosphere, with less emphasis on soil moisture. However, when PM 10 concentrations were high, soil moisture was most important in discerning days of very high concentrations on the Arizona side of the border during the most problematic seasons of fall and winter. This was not the case on the Sonora side. Furthermore, drier soil conditions were linked to anomalies in PM 10 on the Arizona side of Nogales that were higher than the corresponding anomaly on the Sonora side. The generation of PM on the Sonora side is less reliant on dry soil than it is on the Arizona side, indicating a higher level of anthropogenic dust production on the Sonora side.
KEY WORDS: Particulate matter · Dust · Synoptic climatology · Soil moisture
Resale or republication not permitted without written consent of the publisherClim Res 30: [113][114][115][116][117][118][119][120][121][122][123][124] 2006 modification (Tegen & Fung 1995), and vehicle traffic flows (Vernath et al. 2003).Estimates of so-called 'fugitive dust' indicate that up to half of the current global atmospheric dust load originates from anthropogenically disturbed soils (Tegen et al. 2004). However, efforts to model world dust emissions from the surface have produced varying estimates of the total load from anthropogenic sources. Sokolik & Toon (1996) estimated an amount of near 20%, while Tegen & Fung (1995) determined a contribution from anthropogenic aerosols between 30 and 50%.In arid regions, where dry soil, a stagnant atmosphere, and population increases associated with an attractive climate can lead to an expansion of dust sources, mitigation efforts are especially important. Regional studies in arid environments have tended to focus on the impact of fugitive dust in areas surrounding road surfaces and restoration of farmland in desert locales. Etyemezian et al. (2004) analyzed the transport of fugitive dust, PM 10 in particular, and found varying degrees of removal of sediment from unpaved road surfaces. The variability in measurements at set distances from the road surfaces were impacted by the atmospheric conditions, which controlled the amount and distance that the dust was transported. A similar study by Vernath et al. (2003) also noted the decrease in concentratio...