Rm. Hoff et al., LIDAR, NEPHELOMETER, AND IN-SITU AEROSOL EXPERIMENTS IN SOUTHERN ONTARIO, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D14), 1996, pp. 19199-19209
During August 1992, a complex aerosol and optical experiment was perfo
rmed at Egbert, Ontario, Canada. In situ data from Berner impactors, t
hree active scattering aerosol spectrometer probes, a differential mob
ility analyzer, filter, and denuder samples were intercompared with op
tical measurements from a nephelometer and a lidar. A haze event durin
g the study period has been modeled using the measured in situ particl
e size data and a hygroscopic growth model. Agreement between the mode
led and the measured data is good, except in periods of relative humid
ities in excess of 90%. Explosive particle growth during the midmornin
g hours is explained by gas-particle conversion processes of sulphur-b
earing species. The light scattering measurements lead to a specific s
cattering coefficient of the dry aerosol of 3.2 m(2) g(-1), but the re
sult is clearly dependent on air mass origin and relative humidity. Th
e latter result is important in global models of radiative response to
anthropogenic aerosol inputs (sulphate aerosol, lidar, nephelometer,
light scattering, aerosol radiative forcing).