Rj. Weber et al., Measurements of enhanced H2SO4 and 3-4 nm particles near a frontal cloud during the First Aerosol Characterization Experiment (ACE 1), J GEO RES-A, 106(D20), 2001, pp. 24107-24117
Observations of new particle production recorded near a frontal cloud at si
milar to6 km above sea level in a remote marine region are reported. Two di
stinct locations situated near the cloud were found to have enhanced concen
trations of sulfuric acid vapor (H2SO4) and freshly formed 3-4 nm particles
. Both were in droplet-free air situated above cloudy regions. No evidence
for enhanced H2SO4 or nucleation was observed in clear air far from the clo
ud. In the nucleating region the aerosol size distribution from 3 nm to 600
mum was observed to be trimodal, with a prominent ultrafine mode, and was
qualitatively, similar to surface-based measurements recorded in regions of
postfrontal subsidence. The measurements support the notion that new parti
cle production in the free troposphere occurs preferentially in clear air n
ear clouds via enhanced photochemical production of nucleation precursor ga
ses and that H2SO4 participates. A model simulation suggested that a doubli
ng of ultraviolet intensities above the cloud due to cloud enhanced up-well
ing radiation or reasonable enhancements in sulfur dioxide concentrations c
ould account for the higher H2SO4 concentration observed near the cloud. In
the nucleation regions, H2SO4 and water vapor concentrations were too low
for binary nucleation of sulfuric acid and water, according to current nucl
eation models. The mechanisms of particle formation and growth remain uncer
tain. The measurements were part of the first Aerosol Characterization Expe
riment (ACE 1) conducted in the remote South Pacific Ocean (153 degreesE, 4
7 degreesS) on November 27, 1995.