Some 30 years of physical and chemical marine aerosol data are reviewed to
derive global-size distribution parameters and inorganic particle compositi
on on a coarse 15 degrees x 15 degrees grid. There are large gaps in geogra
phical and seasonal coverage and chemical and physical aerosol characterisa
tion. About 28% of the grid cells contain physical data while there are com
positional data in some 60% of the cells. The size distribution data were p
arametrized in terms of 2 submicrometer log-normal distributions. The spars
eness of the data did not allow zonal differentiation of the distributions.
By segregating the chemical data according to the major aerosol sources, s
ea salt, dimethylsulfide, crustal material, combustion processes and other
anthropogenic sources, much information on mass concentrations and contribu
tion of natural and anthropogenic sources to the marine aerosol can be glea
ned from the data base. There are significant meridional differences in the
contributions of the different sources to the marine aerosol. Very clearly
, we see though that the global marine surface atmosphere is polluted by an
thropogenic sulfur. Only in the case of sulfur components did the coverage
allow the presentation of very coarse seasonal distributions which reflect
the spring blooms in the appropriate parts of the oceans. As an example of
the potential value in comparing the marine aerosol data base to chemical t
ransport models, global seasonal meridional MSA distributions were compared
to modelled MSA distributions. The general good agreement in mass concentr
ations is encouraging while some latitudinal discrepancies warrant further
investigations covering other aerosol components such as black carbon and m
etals.