TY - JOUR
T1 - Effects of local pollution and environmental humidity on aerosol-size spectra and light-scattering coefficients in southern Taiwan
AU - Lee, Chung Te
AU - Hsu, Wen Chuan
N1 - Funding Information:
Acknowledgment-The authors acknowledge financial support from the National Science Council in Taiwan (R.O.C.) under Grant NSC 85-2621-P-008-006.
PY - 1999/5
Y1 - 1999/5
N2 - Atmospheric aerosols were intensively studied in Tainan in southern Taiwan from February to March 1995. The time-series data showed that variations of hourly aerosol light-scattering coefficients (σ(scat)) and aerosol volume concentrations were consistent with a squared correlation coefficient at 0.87. For comparisons with the measured σ(scat), the aerosol light-scattering coefficient was calculated (σ(scat, c)) using the Mie theory and aerosol size spectra. A linear regression analysis showed that the squared correlation coefficient between σ(scat, c) and σ(scat) was at 0.89. During the study period, certain events were observed which might result from variations of either meteorology or source emissions. The morning fog was found to have the most progressive growth in the range of 0.8 to 0.9 μm, with a minor contribution from a size interval of 1 to 2 μm. In contrast, other activities showed the most progressive size interval was from 0.35 to 0.6 μm. In this study, two cases affected predominantly by the variations in relative humidity (RH) were chosen to investigate the σ(scat, c) across aerosol sizes. In an ascending RH environment, the σ(scat) increased from 0.35 to 0.50 km-1 with an increasing σ(scat, c) in the range from 0.2 to 0.9 μm. For a descending RH environment, the σ(scat) reduced from 0.75 to 0.14 km-1 with a significant reduction in σ(scat, c) for the range from 0.45 to 2.0 μm.
AB - Atmospheric aerosols were intensively studied in Tainan in southern Taiwan from February to March 1995. The time-series data showed that variations of hourly aerosol light-scattering coefficients (σ(scat)) and aerosol volume concentrations were consistent with a squared correlation coefficient at 0.87. For comparisons with the measured σ(scat), the aerosol light-scattering coefficient was calculated (σ(scat, c)) using the Mie theory and aerosol size spectra. A linear regression analysis showed that the squared correlation coefficient between σ(scat, c) and σ(scat) was at 0.89. During the study period, certain events were observed which might result from variations of either meteorology or source emissions. The morning fog was found to have the most progressive growth in the range of 0.8 to 0.9 μm, with a minor contribution from a size interval of 1 to 2 μm. In contrast, other activities showed the most progressive size interval was from 0.35 to 0.6 μm. In this study, two cases affected predominantly by the variations in relative humidity (RH) were chosen to investigate the σ(scat, c) across aerosol sizes. In an ascending RH environment, the σ(scat) increased from 0.35 to 0.50 km-1 with an increasing σ(scat, c) in the range from 0.2 to 0.9 μm. For a descending RH environment, the σ(scat) reduced from 0.75 to 0.14 km-1 with a significant reduction in σ(scat, c) for the range from 0.45 to 2.0 μm.
UR - http://www.scopus.com/inward/record.url?scp=0033136415&partnerID=8YFLogxK
U2 - 10.1016/S0160-4120(99)00013-6
DO - 10.1016/S0160-4120(99)00013-6
M3 - 期刊論文
AN - SCOPUS:0033136415
SN - 0160-4120
VL - 25
SP - 433
EP - 441
JO - Environment International
JF - Environment International
IS - 4
ER -