Abstract
Natural and artificial snowflakes have been rimed both in free fall and while suspended on a thin flexible fiber in the UCLA cloud tunnel. The results of these experiments show that during the early stage of riming, the motions exhibited by a riming aggregated do not affect the distribution of the rime accretion, in agreement with the observations of the riming behaviour of porous ice disks, reported in Part I of this study. It was also found that the collection kernel of a 10-mm diameter porous aggregate increased with respect to porosity at the same rate as that in Part I of this study. A discussion is presented of the free-fall behavior and the time evolution of the terminal velocities of riming aggregats.-Authors
| Original language | English |
|---|---|
| Pages (from-to) | 2410-2417 |
| Number of pages | 8 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 43 |
| Issue number | 21 |
| DOIs | |
| State | Published - 1986 |
| Externally published | Yes |