The oscillatory angular motion of the snowflake is determined by a stereophotographic technique, in order to investigate the effect of the orientation of a falling snow particle on its collection efficiency.
The results are summerized as follows
1) The frequency distribution of the amplitude of oscillatory angular motion extends to about 35° but the modal amplitude lies in the region from 0° to 5°.
2) Frequency distributions of the angular velocities both about the vertical and the horizontal axis are bimodal type.
3) In the frequency distribution of the angular velocity about the vertical axis, the first modal velocity lies in the range less than 2.5 rad/sec and the second in 7.5 rad/sec to 10 rad/sec. Their mean velocity is 3.45 rad/sec.
The angular velocity less than 2.5 rad/sec has a frequency of occurrence larger than 50% and the angular velocity less than 5.0 rad/sec has one larger than 88%.
4) In the distribution of angular velocity about the horizontal axis, the first modal velocity lies in the range from 5.0 rad/sec to 7.5 rad/sec and the second in the range from 17.5 rad/sec 20.0 rad/sec. The mean velocity is 9.85 rad/sec and is about 3 times that about the vertical axis.
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