## Abstract I t is generally acknowledged that superβcooled water drops can exist at temperatures far below freezing and are of common occurrence in cloud. In many cases, therefore, it is to be expected that a s saturated air rises, as for instance in a large cumulus cloud, its surplus water vapour
The adiabatic lapse-rate for dry and saturated air
β Scribed by D. Brunt
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 542 KB
- Volume
- 59
- Category
- Article
- ISSN
- 0035-9009
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