The Program for Research on Oxidants: Photochemistry, Emissions, and Transp
ort (PROPHET) summer 1998 measurements intensive was conducted from a tower
above a forested site in northern Michigan. This paper provides a brief ov
erview of the meteorological conditions and establishes that the study peri
od was moderately drier and warmer than the climatological mean. The paper
also identifies and chemically characterizes the major air mass types influ
encing the site. Meteorological analyses and back trajectories establish th
at air mass origin oscillated between relatively clean Canadian regions (ex
cept for periods influenced by Canadian forest fires) and regions of greate
r anthropogenic emissions in the contiguous United States. Higher mixing ra
tios of ozone, CO, NOx and NOz were generally associated with southerly tra
nsport, which occurred 24% of the time. Lower mixing ratios were observed u
nder northerly transport, which occurred 44% of the time. The dominance of
northerly transport was due to a stronger than normal Hudson Bay low. The r
emaining 32% of the time was occupied by,transitional periods between disti
nct air masses. A positive slope exists between ozone and CO when photochem
ically aged air masses are selected. However, no meaningful relationship be
tween ozone and CO was observed when northerly and southerly transport peri
ods were considered separately. Comparison to other summertime rural locati
ons suggests that rapid and frequent transitions between air masses of cont
rasting source regions play an important role in maintaining the 0.3 O-3/CO
slope commonly observed in eastern North America.