Abstract
Measurements obtained in a thin, cirriform cloud that formed in the temperature range -83o to -84oC and an altitude range at 16.2 to 16.7 are presented. Implications of the results for particle generation in polar stratospheric clouds developing with similar conditions are discussed.-Author
| Original language | English |
|---|---|
| Pages (from-to) | 851-855 |
| Number of pages | 5 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 43 |
| Issue number | 8 |
| DOIs | |
| State | Published - 1986 |
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