Tropospheric aerosols affect the radiative forcing of Earth's climate, but
their variable concentrations complicate an understanding of their global i
nfluence. Model-based estimates of aerosol distributions helped reveal spat
ial patterns indicative of the presence of tropospheric aerosols in the sat
ellite-observed clear-sky solar radiation budget over the world's oceans. T
he results show that, although geographical signatures due to both natural
and anthropogenic aerosols are manifest in the satellite observations, the
naturally occurring sea-salt is the leading aerosol contributor to the glob
al-mean dear-sky radiation balance over oceans.