We employ the Geophysical Fluid Dynamics Laboratory (GFDL) global chemistry
transport model (GCTM) address the episodic nature of trans-Pacific pollut
ion. The strongest Asian CO episodes over North America (NA), occurring mos
t frequently between February and May, are often associated with disturbanc
es that entrain pollution over eastern Asia and amplify over the western Pa
cific Ocean. Using 55 ppb of Asian CO as a criterion for major events, we f
ind that during a typical year three to five Asian pollution events analogo
us to those observed by Jaffe et al. [1999] are expected in the boundary la
yer all along the U.S. West Coast between February and May. Tn contrast to
CO, Asia currently has a small impact on the magnitude and variability of b
ackground ozone arriving over NA from the west. Direct and indirect Asian c
ontributions to episodic O-3 events over the western United States are gene
rally in the 3 - 10 pphv range. The two largest total O-3 events (>60 pphv)
, while having trajectories which pass over Asia, show negligible impact fr
om Asian emissions. However, this may change. A future emission scenario, i
n which Asian NOx emissions increase by a factor of 4 from those in 1990 pr
oduces late spring ozone episodes at the surface of California with Asian c
ontributions reaching 40 ppb. Such episodic contributions are certain to ex
acerbate local NA pollution events, especially in elevated areas more frequ
ently exposed to free tropospheric and more heavily Asian -influenced air.