Abstract
Ice particle concentrations have been measured from the NOAA/NCAR Explorer sailplane in unmixed and mixed updraft regions within northeast Colorado cumulus congestus clouds, and compared with the concentrations predicted from measured ice nucleus spectra. The concentrations of ice particles within unmixed updraft regions, exclusive of ice particles so large that they almost certainly entered the unmixed region by sedimentation or recycling, are consistent with those expected on the basis of the ice nucleus spectra, suggesting that primary ice nucleation is the dominant mechanism active within these regions. The data do not indicate an important role for ice multiplication in these clouds.- from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 2216-2229 |
| Number of pages | 14 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 36 |
| Issue number | 11 |
| DOIs | |
| State | Published - 1979 |