During the spring of 1998, smoke produced by biomass burning in Central Ame
rica was transported northward, where it eventually affected the continenta
l United States. To quantify this event, this study analyzes the presence o
f aerosols using the Total Ozone Mapping Spectrometer (TOMS) aerosol index.
Unusually large amounts of UV-absorbing aerosols were present over parts o
f Central America during 1998 compared to a climatology created from the 13
-year Nimbus 7 TOMS data set (1979-1992). The role of transport is studied
by computing trajectories for air parcels initialized in the area with the
most widespread fires. Comparison of the TOMS aerosol index maps and the pa
rcel trajectories indicates that the trajectories adequately represent the
smoke transport. Analysis of the TOMS data, the meteorological observations
, and the trajectories indicates that the source region of the smoke is inf
luenced by two prevailing transport regimes: one northward and one westward
. The transport alternates between the two flow patterns. Statistical analy
sis of the transport shows that May 1998 and the climatology contain simila
r patterns of northward and westward flow regimes. The northward flow regim
e in 1998, however, is among the strongest of the 20-year period analyzed.
The combination of unusually large smoke production and stronger than norma
l northward transport led to significant smoke concentrations over large ar
eas of the central and southern United States.