In this paper we investigate the aerosol content retrieved by Earth-Probe T
otal Ozone Mapping Spectrometer (TOMS) and ADEOS POLDER over oceanic region
s for the period November 1996 to June 1997. We combine the aerosol index (
AI) derived from TOMS corresponding to UV-absorbing aerosols (desert dust a
nd biomass-burning particles) and the POLDER aerosol optical thickness (AOT
) and Angstrom coefficients. The seasonal composited images from the two se
nsors show in general consistent spatial distributions of the aerosol over
oceans, with the highest aerosol content retrieved over the north tropical
and equatorial Atlantic. Over the different oceanic regions investigated (i
.e., Atlantic Ocean, Mediterranean Sea, Indian Ocean, and Pacific Ocean), T
OMS and POLDER show a good correspondence in the aerosol seasonal variabili
ty. At all sites with the exception of the region of the Sea of Japan, we s
how that during the time periods of maximum aerosol amounts, a linear corre
lation exists between the TOMS AI and POLDER AOT. For the Sea of Japan the
influence of different aerosol types (i.e., desert dust and sulfates) is li
kely to complicate the TOMS detection. For the other oceanic regions, our r
esults suggest a large variability in the relationship between the TOMS Al
and the POLDER AOT, which is likely to be related to changes in aerosol com
position and/or altitude.