Is. Mcdermid et Td. Walsh, SURFACE OZONE LEVELS AT TABLE MOUNTAIN DURING STOIC 1989, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 100(D5), 1995, pp. 9301-9302
As a part of the routine operations of the Jet Propulsion Laboratory a
tmospheric measurements program at the Table Mountain Facility, the su
rface ozone concentration is continuously monitored using a Dasibi pho
tometer. The influence of the Los Angeles basin to the southwest of th
e facility and the height of the inversion layer cause large fluctuati
ons in the ozone concentration, Peaks as high as 200 parts per billion
by volume (ppbv) were observed during the Stratospheric Ozone Interco
mparison Campaign (STOIC) compared to a normal background level near 5
0 ppbv. These measurements, made during STOIC, were important in asses
sing the impact of the surface ozone concentration on the various inst
ruments participating in the campaign.