Is. Kristament et al., A SEASONAL CYCLE IN THE SOUTHWEST PACIFIC FREE TROPOSPHERIC AEROSOL CONCENTRATION, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 98(D9), 1993, pp. 16829-16837
Measurements made of the concentration of aerosol particles in the dia
meter range 0.15 - 3mum in the free troposphere over the southwest Pac
ific show evidence of a seasonal cycle. The maximum concentration occu
rs in spring and the minimum in autumn. The amplitude of the cycle is
greatest at 30-degrees-S where, in early spring, the mean aerosol conc
entration is 18 cm-3, more than 10 times the mean autumn value. In the
vicinity of the equator die seasonality disappears and concentrations
throughout die year apparently remain close to the autumn levels at o
ther latitudes. A number of different mechanisms could account for the
observed seasonality but it is probable that die peak in early spring
is due to biomass burning through the tropical southern hemisphere dr
y season. Continued high values through late spring and early summer a
re thought to be the result of die seasonal production of aerosol prec
ursors, such as dimethyl sulfide (DMS), at middle and high latitudes.