Abstract

Abstract. The North China Plain (NCP) has become one of the most polluted regions in China, with the rapidly increasing economic growth in the past decades. High concentrations of ambient O3 and aerosol have been observed at urban as well as rural sites in the NCP. Most of the in situ observations of air pollutants have been conducted near the ground so that current knowledge about the vertical distributions of tropospheric O3 and aerosol over the NCP region is still limited. In this study, vertical profiles of O3 and size-resolved aerosol concentrations below 2.5 km were measured in summer 2014 over a rural site in the NCP, using an unmanned aerial vehicle (UAV) equipped with miniature analyzers. In addition, vertical profiles of aerosol scattering property in the lower troposphere and vertical profiles of O3 below 1 km were also observed at the site using a lidar and tethered balloon, respectively. The depths of the mixed layer and residual layer were determined according to the vertical gradients of lidar particle extinction and aerosol number concentration. Average O3 and size-resolved aerosol number concentration in both the mixed and residual layer were obtained from the data observed in seven UAV flights. The results show that during most of the flights the O3 levels above the top of mixed layer were higher than those below. Such a positive gradient in the vertical distribution of O3 makes the residual layer an important source of O3 in the mixed layer, particularly during the morning when the top of mixed layer is rapidly elevated. In contrast to O3, aerosol number concentration was normally higher in the mixed layer than in the residual layer, particularly in the early morning. Aerosol particles were overwhelmingly distributed in the size range < 1 µm, showing slight differences between the mixed and residual layers. Our measurements confirm that the lower troposphere over the rural area of the NCP is largely impacted by anthropogenic pollutants locally emitted or transported from urban areas. Compared with the historic O3 vertical profiles over Beijing from the Measurement of Ozone and Water Vapor by Airbus In-Service Aircraft (MOZAIC), a strong increase in O3 can be found at all heights below 2.5 km in the decade from 2004 to 2014, with the largest enhancement of about 41.6 ppb. This indicates that the lower troposphere over the northern part of the NCP has experienced rapidly worsening photochemical pollution. This worsening trend in photochemical pollution deserves more attention in the future.

Highlights

  • Ozone (O3) is a key trace gas and oxidant in the troposphere, which can generate hydroxyl radical (OH), which affects the oxidizing capacity of the atmosphere

  • The vertical profiles of O3 were acquired during seven unmanned aerial vehicle (UAV) flights as listed in Table 1, while aerosol number concentrations in six size bins were observed during five of the seven flights

  • Vertical profiles of particle extinction property, O3, and size-resolved aerosol concentration were simultaneously measured using miniature devices installed in an UAV over a rural site in the North China Plain (NCP) during the summer of 2014, allowing for the characterization of diurnal O3 and aerosol concentration in mixing layer and residual layer over a small area

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Summary

Introduction

Ozone (O3) is a key trace gas and oxidant in the troposphere, which can generate hydroxyl radical (OH), which affects the oxidizing capacity of the atmosphere. Knowledge of this aspect is important for atmospheric chemistry and physics studies. There is only limited knowledge of the vertical distributions of tropospheric O3 and aerosol over the NCP region, gained in some sporadic observational studies (Chen et al, 2009, 2013; Ma et al, 2011; Wang et al, 2012; Zheng et al, 2005) This hinders extensive validations of atmospheric chemistry models as well as the assessment of climate effects of O3 and aerosols over this important region. To the best of our knowledge, there has been no similar published study of the region of China

Ground-based measurements
Flight information
Results and discussion
Determination of the mixed and residual layer depth
Average O3 and aerosol number concentrations in the mixed and residual layers
Comparison with historic O3 vertical profiles
Conclusion
Full Text
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