Compendium of meteorology. Meteorology. THE PHYSICS OF ICE CLOUDS AND MIXED CLOUDS 193 small ice-supersatiirations). Fournier d'Albe [9] pro- duced these particles bj'- evaporating crystals which had been grown at —41C

Download this stock image: . Compendium of meteorology. Meteorology. THE PHYSICS OF ICE CLOUDS AND MIXED CLOUDS 193 small ice-supersatiirations). Fournier d'Albe [9] pro- duced these particles bj'- evaporating crystals which had been grown at —41C in the presence of solution droplets of cadmium iodide. It seems likely that the particles remaining consisted of cadmiimi iodide bearing microfilms of water which retained an icelike structure such as cannot be imposed upon films adsorbed from the vapour, even by cooling to temperatures in the neigh- bourhood of — 70C. This suggests that the only sublima- tion nuclei are in f - REDXR3 from Alamy's library of millions of high resolution stock photos, illustrations and vectors.
. Compendium of meteorology. Meteorology. THE PHYSICS OF ICE CLOUDS AND MIXED CLOUDS 193 small ice-supersatiirations). Fournier d'Albe [9] pro- duced these particles bj'- evaporating crystals which had been grown at —41C in the presence of solution droplets of cadmium iodide. It seems likely that the particles remaining consisted of cadmiimi iodide bearing microfilms of water which retained an icelike structure such as cannot be imposed upon films adsorbed from the vapour, even by cooling to temperatures in the neigh- bourhood of — 70C. This suggests that the only sublima- tion nuclei are in f

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. Compendium of meteorology. Meteorology. WATER VAPOUR IN THE UPPER AIR 313 lower than 180K. Thus if the thimble should be cooled below this temperature, the ice will form as a glassy- layer which scatters no light. In using the eye-observation

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