Abstract
Both gram-positive and gram-negative bacteria become excellent condensation nuclei when lyophilized to dryness. The same freeze-dry procedure does not inactivate the highly effective freezing nuclei produced by ice nucleation active bacteria. Therefore, irrespective of their contact nucleation potential, ice nucleation-active bacteria ought to effect condensation freezing at −10°C of warmer in cloud systems. Output from a numerical cloud model suggests that the condensation freezing capability of ice nucleation-active bacteria at warmer temperatures could be exploited to produce rainfall from clouds too warm to respond positively to inorganic nucleants like silver iodide.
Original language | English |
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Pages (from-to) | 1188-1197 |
Number of pages | 10 |
Journal | Journal of Applied Meteorology and Climatology |
Volume | 26 |
Issue number | 9 |
DOIs | |
State | Published - 1 Sep 1987 |