Abstract

Abstract. Long-term measurements of particle number size distributions were carried out both at an urban background site (Peking University, PKU) and a regional Global Atmospheric Watch station (Shangdianzi, SDZ) from March to November in 2008. In total, 52 new particle formation (NPF) events were observed simultaneously at both sites, indicating that this is a regional phenomenon in the North China Plain. On average, the mean condensation sink value before the nucleation events started was 0.025 s−1 in the urban environment, which was 1.6 times higher than that at regional site. However, higher particle formation and growth rates were observed at PKU (10.8 cm−3 s−1 and 5.2 nm h−1) compared with those at SDZ (4.9 cm−3 s−1 and 4.0 nm h−1). These results implied that precursors were much more abundant in the polluted urban environment. Different from the observations in cleaner environments, the background conditions of the observed particle homogeneous nucleation events in the North China Plain could be characterized as the co-existing of a stronger source of precursor gases and a higher condensational sink of pre-existing aerosol particles. Secondary aerosol formation following nucleation events results in an increase of particle mass concentration, particle light scattering coefficient, and cloud condensation nuclei (CCN) number concentration, with consequences on visibility, radiative effects, and air quality. Typical regional NPF events with significant particle nucleation rates and subsequent particle growth over a sufficiently long time period at both sites were chosen to investigate the influence of NPF on the number concentration of "potential" CCN. As a result, the NPF and the subsequent condensable growth increased the CCN number concentration in the North China Plain by factors in the range from 5.6 to 8.7. Moreover, the potential contribution of anthropogenic emissions to the CCN number concentration was more than 50%, to which more attention should be drawn in regional and global climate modeling, especially in the polluted urban areas.

Highlights

  • Impacts of aerosol particles on the earth–atmosphere system, including the climate, ecosystem, air quality and public health, determine its highlighted topics in atmospheric environmental research (IPCC, 2007)

  • The results showed that the typical particle growth rates in nucleation mode range from 1 to 20 nm h−1 in mid-latitudes, whereas particle formation rates vary widely depending on the air mass type of sampling site

  • For several days with the New particle formation (NPF) event shown at PKU, we only observed a similar particle growth pattern at SDZ

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Summary

Introduction

Impacts of aerosol particles on the earth–atmosphere system, including the climate, ecosystem, air quality and public health, determine its highlighted topics in atmospheric environmental research (IPCC, 2007). The NPF events had been observed in a marine area (Lin et al, 2007), high-elevation mountains (Guo et al, 2012; Kivekas et al, 2009; Li et al, 2011), rural sites of Pearl River delta (Liu et al, 2008; Wang et al, 2013c), suburban environments in Yangtze River delta region (Gao et al, 2009; Herrmann et al, 2013) and Lanzhou (Gao et al, 2011), as well as urban Shanghai (Du et al, 2012) These observations were independent and only based on short-term observations. The characteristics are compared, and the influences of NPF events on the direct (particle light scattering coefficient) and indirect (CCN number concentration) aerosol effects are evaluated

Sampling site
Instrumentation
Classification scheme
Occurrence of new particle formation event
Influences on the light scattering and CCN
Conclusions
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