W. Szyrmer et I. Zawadzki, BIOGENIC AND ANTHROPOGENIC SOURCES OF ICE-FORMING NUCLEI - A REVIEW, Bulletin of the American Meteorological Society, 78(2), 1997, pp. 209-228
To develop theories and numerical models of the formation and microstr
ucture of clouds and precipitation, it is necessary to identify the po
tential sources of ice nuclei in the atmosphere. However, the subject
remains an area of debate. According to the most accepted theory, the
great majority of atmospheric ice nuclei constitute soil mineral parti
cles. But some evidence appears to favor the hypothesis of a nonneglig
ible contribution to the population of effective ice nuclei made by bi
ogenic material, living or dead. Moreover, some specific human activit
ies have been identified as prolific sources of particles on which ice
crystals can be generated. In contrast, it has also been suggested th
at some anthropogenic effluents deactivate nuclei naturally occurring
in the atmosphere. This paper summarizes present knowledge about the b
iogenic and anthropogenic sources of atmospheric ice nuclei. Recent re
search reveals an increasingly greater variety of sources and activiti
es of ice nuclei. However intriguing and potentially significant these
findings are, the overall picture emerging from the review is one of
inconclusive, and sometimes contradictory, results. A standarization o
f measurement techniques and a more coordinated and systematic effort
in the search for a general theory of heterogeneous ice nucleation are
needed to answer the fundamental questions, what is the origin of atm
ospheric ice nuclei, and what is their activity spectrum?.