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Title: Anomalous snowfall caused by natural-draft cooling towers

Technical Report ·
DOI:https://doi.org/10.2172/5249059· OSTI ID:5249059

Scattered reports of significant amounts of snow anomalously produced by cooling-tower plumes suggest that this process may be of importance. This conclusion is supported by study of high-resolution satellite images. Tabulation of a number of aerial observations of plumes at subfreezing temperatures indicates that a plume is likely to produce measurable snow if its temperature is colder than -13/sup 0/C and the saturation deficit of the ambient air is less than 0.5 g m/sup -3/. These factors are important because they affect the rates of nucleation and growth of ice particles. The rate of mixing between plume and ambient air is also important because it affects the rate of evaporation within the plume, which in turn determines the length of time available for snow particles to grow large enough to fall out. These empirically derived criteria were tested using a numerical model of cloud microphysics that simulates the most important processes of transfer of water substance between vapor, liquid, and ice, including nucleation and development of particle-size spectra. Dynamic processes were specified, not modeled. Among the many quantities computed is the flux density of snow at the base of the plume. From this, together with average fallspeed and horizontal wind speed, one can compute the amount and pattern of snowfall at the ground.

Research Organization:
RAND Corp., Santa Monica, CA (United States)
DOE Contract Number:
AC03-76EV01191
OSTI ID:
5249059
Report Number(s):
RAND/N-1479-DOE; TRN: 80-012244
Country of Publication:
United States
Language:
English