Ultrafine (< 100 nm) aerosol particles, emitted
during
combustion and generated from atmospheric chemical reactions, are
important to
both human health and climate. Thanks to
more widespread use of ultrafine particle counters and Scanning
Mobility
Particle Sizing, ambient measurements of these particles at high (~5
min) time
resolution are becoming increasingly common.
At the University
of Iowa, we have
developed tools to organize and analyze size distribution data from
multiple
locations, together with collocated meteorological, gas-phase, and
aerosol-phase data. Both tools and
analysis results will be discussed, using datasets from the USEPA
Particulate
Matter Supersites Program, Bondville Illinois,
the MILAGRO field campaign, the Southern California PM Center, and
other
studies.
In terms of results, we will present summary
statistics
regarding ultrafine particles at these locations, the measured
occurrence of
new particle formation at these locations, and the impact of vehicular
emission
on each of the measured sites. For
example, the Pittsburgh
site had an average number concentration (3-500 nm) of 22,000 cm-3
with an average number mode of 40 nm. Regional
new particle formation events are most common in Pittsburgh (~3 of 10 days averaged
over 1
year). Sampling duration was not long
enough in Bondville (2 months) or Mexico City (1 month) to establish an
overall
frequency, but particle formation events appear to be somewhat less
frequent
(than Pittsburgh) in both locations. In Mexico City, the
role of
the boundary layer and residual layer in new particle formation appears
to be
very important. The Mexico City basin has been shown to
have
strong thermally and topographically driven circulations.
The connection of this unique meteorology to
new particle formation is potentially important and may help to rule
out some
mechanisms for new particle formation. On
several of the study days in Mexico
City, rapid decreases in PM concentrations in
the
early afternoon are simultaneous with rapid increase in boundary layer
height,
high friction velocities, and the appearance of a newly formed and
growing
sub-50 nm mode in the number size distribution.
The following data analysis problems will be
discussed:
separating local-source combustion ultrafines from new particle
formation,
integrating data and deterministic models of vehicle and atmospheric
ultrafine
particles, and using CO2 and particle size distribution time
series.