Gh. Mount et Ej. Williams, AN OVERVIEW OF THE TROPOSPHERIC OH PHOTOCHEMISTRY EXPERIMENT, FRITZ-PEAK IDAHO-HILL, COLORADO, FALL 1993, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 102(D5), 1997, pp. 6171-6186
`An extensive study of tropospheric photochemical trace species, inclu
ding the hydroxyl radical OH was conducted in the Colorado Rocky Mount
ains from early August to early October 1993. Many of the parameters t
hat influence the abundance of OH in the atmosphere, including j(O-3 a
nd NO2), formaldehyde, nonmethane hydrocarbons, NOx, ozone, H2O, aeros
ols, and others, were measured simultaneously with OH. Instrumentation
for measurement of OH included a long-path spectroscopic technique an
d several in situ techniques: ion-assisted mass spectrometry, laser-in
duced resonance fluorescence, and a liquid scrubber/liquid chromatogra
phic method. Instrument comparisons between long-path and in situ meas
urements were conducted for OH, O-3, CH2O, NO2, and H2O, and these mea
surements provide a valuable insight into the chemistry of the region.
The complete data set provided a robust set of inputs to a zero-dimen
sional model for exploring OH photochemistry. Independently measured O
H concentrations were in agreement within one standard error much of t
he time, thus giving confidence that hydroxyl is being measured correc
tly. OH concentrations were typically low during clean continental air
flow with concentrations rarely above 4 x 10(6) cm(-3). During occasio
ns of polluted airflow from the Denver-Boulder metropolitan areas, val
ues of OH rose as high as 1.2 x 10(7) cm(-3). The nearly complete suit
e of trace gases measured simultaneously with the hydroxyl radical sev
erely constrained the models and provided numerous opportunities to co
mpare relations between species (e.g. OH versus NOx, OH/HO2, RO(2) ver
sus NOx). Modeled hydroxyl results using the complete species suite we
re about a factor of 1.5 higher than measured OH concentrations sugges
ting that the photochemistry may not be well understood. The campaign
data provide new insights into the chemistry of the lower troposphere.
This paper provides an overview of the campaign and brief description
s of results from individual experiments. Details are provided in the
accompanying papers in this issue.