J. Rutllant et R. Garreaud, METEOROLOGICAL AIR-POLLUTION POTENTIAL FOR SANTIAGO, CHILE - TOWARDS AN OBJECTIVE EPISODE FORECASTING, Environmental monitoring and assessment, 34(3), 1995, pp. 223-244
The geography and climate of the Santiago basin are, in general, unfav
orable for the diffusion of air pollutants. Consequently, extreme even
ts occur frequently during the high pollution season extending from Ap
ril to August. The meteorological conditions concurrent with those ext
reme events are mainly associated with the leading edges of coastal lo
ws that bring down the base of the semipermanent temperature inversion
reducing the diurnal growth of the surface mixed layer. Tn order to p
roduce an objective 12 to 24-hour episode forecast, a two-way multivar
iate discriminant analysis has been used in the definition of a meteor
ological air-pollution potential index (MAPPI), separating high and lo
w meteorological air-pollution potential days, The same procedure has
been applied in the selection of the most efficient predictors for the
MAPPI objective forecast, based on 12 and 24 UTC radiosonde data at Q
uintero, about 100 km to the NW of Santiago. Results indicate about 70
% correctly forecasted days, with satisfactory skill-scores relative t
o persistency. The strong persistency characterizing the most efficien
t predictors in the 12-hour objective forecast scheme, makes the predi
ction of the first and last days of any particular air-pollution poten
tial episode particularly difficult. To overcome this problem, a new s
et of predictors based on continuous measurements near the level of th
e top of the temperature inversion layer (900 hPa during air-pollution
episodes) is being tested. Preliminary results indicate that the time
-integrated zonal wind component at that level is a reliable precursor
for both the onset and the end of air-pollution potential episodes.