Abstract

Measurements of the aerosol optical depth (AOD) and the Ångström exponent were retrieved from level 1.5 data obtained by the CE318 sun photometer at Dalian monitoring station from April 2007 to April 2012 to characterize the aerosol spatial and temporal characteristics in this coastal region of Northeast China. The results suggest that the highest mean ± SD value for the AOD over Dalian occurred in the month of July (0.86 ± 0.45), whereas a lower value was observed in the month of January (0.42 ± 0.31). The monthly mean Ångström exponent was at a maximum (about 1.27) in September and October and the minimum value of about 0.60 was recorded in March. The frequency distributions of the AOD and Ångström exponent at Dalian both presented a single peak distribution, with peak values of 0.26 and 1.06, respectively. The scatter grams of the AOD and Ångström exponent suggested that the aerosol size in Dalian was affected by both fine and coarse particles in different seasons. The spectral difference in Ångström exponent wavelength pairs between 440–675 and 675–870 nm indicate that high AOD440 nm values (>1.50) could be clearly identified by the fine mode growth in summer and the addition of coarse mode particles in spring over Dalian. The AOD440 nm value on a foggy day was almost 2.15 times larger than that on a day with high levels of dust. The Ångström exponents (440–870 nm) were about 0.13 and 1.46 on the days with high levels of dust and on the foggy days, respectively.

Highlights

  • Aerosols play an important part in controlling the Earth’s climate because they both absorb and scatter solar radiation

  • The annual mean SD Ångström exponents were 1.17 ̆ 0.30, 1.14 ̆ 0.30, 1.05 ̆ 0.33 and 1.04 ̆ 0.36 in 2008, 2009, 2010 and 2011, respectively, which suggests that the area around the Dalian monitoring station was mainly dominated by small particles

  • This work analyzed the variations in the aerosol optical depth (AOD) and Å ngström exponent retrieved from CE318 sun photometer data from April 2007 to April 2012 over the coastal area of Dalian in Northeast China

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Summary

Introduction

Aerosols play an important part in controlling the Earth’s climate because they both absorb and scatter solar radiation. These processes directly affect the radiation balance between the Earth’s surface and the atmosphere and indirectly affect the climate by their influence on the microphysical processes that take place in clouds [1,2,3,4]. The effects of the optical properties of aerosols on the Earth’s climate have been reported previously [8]. The long-term ground-based monitoring of aerosols is necessary to determine their optical properties [13,14,15,16,17,18]. Networks of ground-based measurements, such as AERONET [19], PHOTONS [20], AEROCAN [21], SKYNET [22]

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