Kk. Moorthy et al., INVESTIGATIONS OF MARINE AEROSOLS OVER THE TROPICAL INDIAN-OCEAN, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 102(D15), 1997, pp. 18827-18842
Results of the studies on the characteristics of marine aerosol optica
l depths made in remote regions of the tropical Indian Ocean using a m
ultiwavelength solar radiometer, taken on a scientific cruise, are pre
sented. The dependence of the aerosol optical depths on prevailing win
ds in marine boundary layer and on deck level relative humidity (RH) a
le examined. Aerosol optical depths (tau(p)) in far oceanic regions wi
th marine air mass prevailing, in general, are found to increase nearl
y exponentially with average wind speed (U-a) as tau(p) = tau(0) exp(a
U-a), where a = 0.16 +/- 0.04. No association is seen with deck level
relative humidity, as the effects of wind appear to offset the effect
s due to RH. The columnar size distributions retrieved from aerosol sp
ectral optical depths reveal two modes, one at similar to 0.04 mu m an
d a secondary mode at similar to 0.8 mu m. The columnar mass loading e
stimated from the size distributions increases exponentially with wind
speed and has a wind independent value of similar to 28 mg m(2).