Abstract

Abstract. Atmospheric aerosol is the primary source of cloud condensation nuclei (CCN). The microphysics and chemical composition of aerosols can affect cloud development and the precipitation process. Among studies conducted in Latin America, only a handful have reported the impact of urban aerosol on CCN activation parameters such as activation ratio (AR) and activation diameter (Dact). With over 20 million inhabitants, the Metropolitan Area of São Paulo (MASP) is the largest megacity in South America. To our knowledge, this is the first study to assess the impact that remote sources and new particle formation (NPF) events have on CCN activation properties in a South American megacity. The measurements were conducted in the MASP between August and September 2014. We measured the CCN within the 0.2–1.0 % range of supersaturation, together with particle number concentration (PNC) and particle number distribution (PND), as well as trace-element concentrations and black carbon (BC). NPF events were identified on 35 % of the sampling days. Combining multivariate analysis in the form of positive matrix factorization (PMF) with an aerosol profile from lidar and HYSPLIT model analyses allowed us to identify the main contribution of vehicular traffic on all days and sea salt and biomass burning from remote regions on 28 and 21 % of the sampling days, respectively. The AR and Dact parameters showed distinct patterns for daytime with intense vehicular traffic and nighttime periods. For example, CCN activation was lower during the daytime than during the nighttime periods, a pattern that was found to be associated mainly with local road-traffic emissions. A decrease in CCN activation was observed on the NPF event days, mainly due to high concentrations of particles with smaller diameters. We also found that aerosols from sea salt, industrial emissions, and biomass burning had minor effects on Dact. For example, nights with biomass burning and vehicular emissions showed slightly lower CCN activation properties than sea-salt, industrial and non-event nights. Our results show that particulate matter from local vehicular emissions during the daytime has a greater effect on CCN activation parameters than that from remote sources.

Highlights

  • Atmospheric aerosol has been the focus of numerous studies, because of its adverse effects on public health and climate (Heal et al, 2012)

  • We evaluated the effects that those air masses associate with local sources and new particle formation (NPF) events had on cloud condensation nuclei (CCN) activation properties

  • The aim of this study was to evaluate the variability in CCN activation parameters under the influence of local sources, remote sources, and NPF, in order to assess the impact of those events on CCN activity in the Metropolitan Area of São Paulo (MASP)

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Summary

Introduction

Atmospheric aerosol has been the focus of numerous studies, because of its adverse effects on public health and climate (Heal et al, 2012). Aerosol particles are a significant source of cloud condensation nuclei (CCN). Owing to their microphysics and chemical composition, aerosol particles can affect cloud development and the precipitation process. The high concentrations of CCN in the air favor the formation of clouds with small droplets, which can lead to suppression of precipitation in shallow and short-lived clouds (Andreae and Rosenfeld, 2008). Such phenomena have been observed at different places. A study carried out in the Brazilian Amazon showed a reduction in precipitation during biomass-burning events, due to greater scavenging from smoky clouds than from clouds formed under clean (blue and green ocean) air masses. The smoky clouds were shown to form at higher altitudes (> 4 km), due to their smaller droplet size, and to produce hydrometeors including isolated intense showers and thunderstorms (Andreae et al, 2004; Freud et al, 2008)

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