The size of the liquid or solid particles in the atmosphere usually extends
from
to
in diameter. In the earth's atmosphere the distribution function which describes
the number of particles as a function of diameter, mass or surface area of the
aerosol can be determined reasonably well with modern instrumentation.
Source:
PAC, 1990, 62, 2167
(Glossary of atmospheric chemistry terms (Recommendations 1990))
on page 2205