Abstract
In February 2001, more than 900,000 high-resolution digital images of ice crystals were recorded at the South Pole using two ground-based cloud particle imagers (CPIs), When sorted by number, 30% of the crystals were rosette shapes, 45% were diamond dust and 25% were irregular-shaped crystals. When sorted by area, rosette shapes comprised 50%, diamond dust 30% and irregulars 20%. By mass, the percentages were 57% rosette shapes, 23% diamond dust and 20% irregulars. In 2002, a polar nephelometer (P-N) that measures scattering phase function was incorporated with one of the CPIs. Particle size distributions as a function of maximum dimension and equivalent radius compared favorably with previous studies.
| Original language | English |
|---|---|
| Pages (from-to) | 1668-1670 |
| Number of pages | 3 |
| Journal | Bulletin of the American Meteorological Society |
| Volume | 87 |
| Issue number | 12 |
| State | Published - Dec 2006 |
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