A yellow sand transport episode from the Asian continent to Japan and North
America which occurred in April 1998 is simulated. A new on-line dust trac
er model coupled with a regional-scale meteorological model is developed an
d applied to this dust storm episode. The results for two large dust events
that started during April 14-15 and 19-20, 1998, have been analyzed and di
scussed. The first dust storm was trapped in a cutoff vortex developed over
the China plain. A modeled 3-D structure of dust associated with this cuto
ff vortex agreed with an observed time-height cross section of dust concent
ration. Results show that the strong subsidence at the backside of the vort
ex restricted the dust layer below 3 km level. Model analysis revealed that
the second dust event that started during April 19-20 over inland China wa
s the origin of a dust episode reported over North America. The trans-Pacif
ic dust transport simulation successfully showed the dust onset near the We
st Coast of North America. Elevation of the dust layer during the long-rang
e transport was below 3 km. The model is extended to include the transport
of an Asian origin anthropogenic tracer over the North Pacific Rim. Both th
e natural-origin mineral dust and the Asian-origin anthropogenic tracer are
simultaneously transported even if their emission regions are different.