Abstract

Ground-based measurements were carried out during field campaigns in April–June of 2010, 2011 and 2012 over northwestern China at Minqin, the Semi-Arid Climate and Environment Observatory of Lanzhou University (SACOL) and Dunhuang. In this study, three dust cases were examined, and the statistical results of dust occurrence, along with physical and optical properties, were analyzed. The results show that both lofted dust layers and near-surface dust layers were characterized by extinction coefficients of 0.25–1.05 km−1 and high particle depolarization ratios (PDRs) of 0.25–0.40 at 527 nm wavelength. During the three campaigns, the frequencies of dust occurrence retrieved from the lidar observations were all higher than 88%, and the highest frequency was in April. The vertical distributions revealed that the maximum height of dust layers typically reached 7.8–9 km or higher. The high intensity of dust layers mostly occurred within the planetary boundary layer (PBL). The monthly averaged PDRs decreased from April to June, which implies a dust load reduction. A comparison of the relationship between the aerosol optical depth at 500 nm (AOD500) and the Angstrom exponent at 440–870 nm (AE440–870) confirms that there is a more complex mixture of dust aerosols with other types of aerosols when the effects of human activities become significant.

Highlights

  • Mineral dust, as a major component of atmospheric aerosols, has a strong impact on the atmosphere [1,2,3,4,5,6]

  • Compared with the distribution of dust at Minqin, there are a number of lofted dust layers above the planetary boundary layer at Dunhuang and SACOL

  • Our results clearly show that both a lofted dust layer and near-surface dust layers were characterized by extinction coefficients of 0.25 to 1.05 km−1 and high particle depolarization ratios (PDRs) of 0.25–0.40 at a 527 nm wavelength

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Summary

Introduction

As a major component of atmospheric aerosols, has a strong impact on the atmosphere [1,2,3,4,5,6]. It affects the radiation budget of the earth’s atmosphere by scattering and absorbing solar radiation, alters cloud characteristics by acting as cloud condensation nuclei or ice nuclei and heats up the surrounding environment [4,6,7,8,9]. Accurately estimating the effects of these factors on radiative forcing by dust aerosols is very difficult

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