## Abstract A method utilizing a vertical wind tunnel is described, by which supercooled water drops and ice particles can be stably suspended at temperatures between 0 and β30Β°C. Using this method, we studied: (i) the freezing temperature of water drops of various purity and volume, (ii) the freez
A wind tunnel investigation of collection kernels for small water drops in air
β Scribed by K. V. Beard; H. R. Pruppacher
- Publisher
- John Wiley and Sons
- Year
- 1971
- Tongue
- English
- Weight
- 469 KB
- Volume
- 97
- Category
- Article
- ISSN
- 0035-9009
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β¦ Synopsis
Abstract
The rate at which small water drops grow by collision and coalescence has been investigated experimentally by means of a wind tunnel constructed for cloud physics research. Individual water drops of radii 70 < A <300ΞΌ were freely suspended in the tunnel airstream carrying a continuous water cloud with droplets of radii 2 < a < 8ΞΌ and with a liquid water content between 0.8 and 1.2 g m^β3^. The rate at which the suspended water drops were growing by collision and coalescence was determined as a function of the drop size of the suspended drop, the liquid water content of the cloud and the size distribution of the drops in the cloud. From the observed parameters, specific collision kernels were computed and compared with those derived from theoretical and experimental collision efficiencies reported in literature. The results show that for p = a/A <0.1, i.e. for large cloud drops growing by collision with small cloud drops, it is justified to compute the growth rate of cloud drops of A < 136ΞΌ on the basis of the theoretical collision efficiencies of Shafrir and Neiburger as given analytically by Berry, and the growth rate of cloud drops of A > 136ΞΌ on the basis of the theoretical collision efficiencies given by Mason.
π SIMILAR VOLUMES
## Abstract The internal circulation and the shape of water drops falling at terminal velocity in air of 20Β°C at sea level pressure, and nearly water saturated, were studied by means of a wind tunnel. Drops with an equivalent radius a~0~ smaller than 140 ΓΌm had within the experimental error no dete