کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
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5754216 | 1620796 | 2017 | 14 صفحه PDF | دانلود رایگان |

The characteristics of springtime aerosols, including their optical and microphysical properties, were analyzed for the months of March to May of 2009 in Gwangju (35.23°N, 126.84°E), Korea. A high Light Detection and Ranging (LIDAR)-derived aerosol depolarization ratio (δ) of 0.25 ± 0.04 was determined on dust particles during the observation period. The à ngström exponent values of the 440-870 nm wavelength pair (à 440-870) and single-scattering albedo at 675 nm (Ω675) measured by a CIMEL sun/sky radiometer were 0.77 ± 0.19 and 0.95 ± 0.01, respectively. The elevated dust layers reached a maximum elevation of 4 km above sea level. Anthropogenic/smoke particles that originated from highly populated/industrialized regions could be distinguished by their relatively smaller particle size (à 440-870 ranged between 1.33 and 1.36) and higher light-absorbing (Ω675 of 0.92 ± 0.01) characteristics. These aerosols are mostly distributed at altitudes < 1.2 km. The root-mean-square deviation (RMSD) between the aerosol optical depth (AOD, Ï) derived from LIDAR (ÏLIDAR) and from the CIMEL sun/sky radiometer (ÏCIMEL) varied with respect to the surface PM10 concentration. The RMSD between ÏLIDAR and ÏCIMEL was as low as 13% under lower PM10 concentration levels (< 100 μg/m3). In contrast, the RMSD between ÏLIDAR and ÏCIMEL increased three times (~ 31%) under high surface PM10 concentration levels (> 100 μg/m3). These results suggest that the accuracy of ÏLIDAR is influenced by specific atmospheric conditions, regardless of its uncertainty.
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Journal: Journal of Environmental Sciences - Volume 57, July 2017, Pages 270-283