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There is hardly a field of science or engineering that does not
have some interest in light scattering by small particles. For
example, this subject is important to climatology because the
energy budget for the Earth's atmosphere is strongly affected by
scattering of solar radiation by cloud and aerosol particles, and
the whole discipline of remote sensing relies largely on analyzing
the parameters of radiation scattered by aerosols, clouds, and
precipitation. The scattering of light by spherical particles can
be easily computed using the conventional Mie theory. However, most
small solid particles encountered in natural and laboratory
conditions have nonspherical shapes. Examples are soot and mineral
aerosols, cirrus cloud particles, snow and frost crystals, ocean
hydrosols, interplanetary and cometary dust grains, and
microorganisms. It is now well known that scattering properties of
nonspherical particles can differ dramatically from those of
"equivalent" (e.g., equal-volume or equal-surface-area) spheres.
Therefore, the ability to accurately compute or measure light
scattering by nonspherical particles in order to clearly understand
the effects of particle nonsphericity on light scattering is very
important. * The first systematic and comprehensive treatment of
electromagnetic scattering by nonspherical particles and its
applications
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