Abstract

Field observations made with unmanned aerial vehicles of the particulate matter (PM) concentration from the ground to a height of 500 m were conducted at Xiaotang and Tazhong in the Taklimakan Desert (TD), China, from 7 to 15 November 2019. The vertical structures of the PM concentrations were studied. Pulsed lidar observations showed that dust aerosols in the TD can reach heights of 4 km. Within 500 m above the ground, the PM1.0, PM2.5, and PM10 concentrations were <100, <201, and <764 µg∙m−3, respectively, in the TD. On days containing sand-blowing periods (e.g., at 18:00 on 11 November), the PM1.0, PM2.5, and PM10 concentrations were 10–17.7 times higher than on clear days. The northern margin of the TD (Xiaotang) was dominated by fine particles, while the hinterland (Tazhong) was dominated by coarse particles, because there was sparse vegetation around Xiaotang and the surface was sand and clay, while there was no vegetation around Tazhong and the surface was sand. During floating dust periods, the boundary layer was dominated by fine particles. The average PM1.0/PM2.5 ratios were 0.25–0.65 and 0.40–0.80 at Tazhong and Xiaotang, respectively, while, during sand blowing periods, these ratios were 0.40–0.55 and 0.40–0.45, respectively. The critical condition in the atmospheric boundary layer for PM concentration was revealed with the enhanced momentum flux and sensible heat flux up to 0.52 kg∙m−1∙s−2, 0.69 m∙s−1, and 6.7 W∙m2, respectively, and the low mixed layer was high in the lower atmosphere.

Highlights

  • Solid and liquid particles suspended in the atmosphere have particle sizes ranging from 10−3 to μm, defined as atmospheric aerosol particles [1]

  • Studies on the dust weather in the Taklimakan Desert (TD) and its surrounding areas have mainly focused on the conditions and changing characteristics of dust weather, as well as the basic spatial and temporal distribution characteristics of dust aerosol PM10 and its influencing factors [1,12,17,29,30,41,42,43,44]

  • We found that the particulate matter (PM) concentrations at Tazhong were closely related to the wind speed and relative humidity (Table 3), while the PM in concentrations Xiaotang were mainly affected by thermal effects (Table 4)

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Summary

Introduction

Solid and liquid particles suspended in the atmosphere have particle sizes ranging from 10−3 to μm, defined as atmospheric aerosol particles [1]. Studies on the dust weather in the TD and its surrounding areas have mainly focused on the conditions and changing characteristics of dust weather, as well as the basic spatial and temporal distribution characteristics of dust aerosol PM10 and its influencing factors [1,12,17,29,30,41,42,43,44] In addition to these studies of particulate matter (PM), some other air pollutants, mainly ozone (O3 ), have been considered, and the results of these investigations have undoubtedly improved our understanding of the vertical characteristics of air pollution in the TD [13,14].

Data and Method
Atmospheric Boundary Layer Conditions
Correlations between the Vertical Profiles in the Hinterland of the TD
Figure
Analysis of the Floating
13. Vertical profiles of the concentrations b
Characteristics of Air Mass Backward Trajectory
Conclusions
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