## Abstract Experiments indicate that secondary ice crystals are produced when rime grows in a supercooled cloud containing drops โฅ 24ฮผm in diameter. This occurs between temperatures of โ3 and โ8ยฐC, the production rate being greatest at โ5ยฐC. These temperatures are constant to about ยฑ0.5 deg C for
The production of showers by the growth of ice particles
โ Scribed by F. H. Ludlam
- Publisher
- John Wiley and Sons
- Year
- 1952
- Tongue
- English
- Weight
- 714 KB
- Volume
- 78
- Category
- Article
- ISSN
- 0035-9009
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โฆ Synopsis
Abstract
A model of cumulusโcloud structure is described, and used, together with the available evidence on the temperatures of iceโcrystal formation and a calculation of the speed of growth of crystals into precipitation elements, to estimate the summitโlevel temperatures at which the formation of showers becomes likely. It appears that in warm weather showers may be expected with summit temperatures of about โ10ยฐC, but in cold weather not until they fall to about โ20ยฐC. Observational evidence is shown to support this view although emphasizing large casual variations, some of whose causes are suggested.
๐ SIMILAR VOLUMES
## Abstract Two series of experiments were undertaken to investigate whether secondary ice particles are thrown off during the accretion of supercooled water drops upon an ice surface. Riming took place in cloud at a temperature of about โ9ยฐC, and the accreted droplets were of various diameters up
## Abstract The production of secondary ice particles when a moving body gathers rime in a supercooled cloud at โ5ยฐC has been studied for various drop size distributions. It is found that the rate of production of ice โsplintersโ depends not only upon the concentration of large drops (โฉพabout 24 ฮผm
## Abstract The growth of unusually large cloud droplets by coalescence within isolated convective clouds is examined. It is found that if their initial radii are about 20 ฮผ or more then growth into raindrops may readily occur. Raindrop nuclei of this size may be provided by spray in maritime air m