## Abstract This paper describes:โ The moisture content of subsiding polar continental air over North America, under conditions when there was no likelihood of an increase in the moisture content due to precipitation from overrunning air. Two situations of this type are discussed, and no evidence
Subsidence and ascent of air as determined by means of the wet-bulb potential temperature
โ Scribed by Richmond W. Longley
- Publisher
- John Wiley and Sons
- Year
- 1942
- Tongue
- English
- Weight
- 796 KB
- Volume
- 68
- Category
- Article
- ISSN
- 0035-9009
No coin nor oath required. For personal study only.
โฆ Synopsis
Abstract
This paper contains:โ
A description of the use of the wetโbulb potential temperature for determining changes in level of air in situations when all levels of the original air column have not the same trajectory;
A derivation of the amount of subsidence which takes place in air moving off the ridge of a high, amounting at times to 1.7 km. in 24 hours from the 3 km. level, and a demonstration of the subsidence of an inversion in the centre of a high of 300 m. in 24 hours;
A demonstration of the overrunning and uplift of a stream of warm air over another stream of colder air;
Some remarks on the divergence of the subsiding air as it moves off the high pressure region;
A discussion of the changes in moisture content which took place in the masses of air considered.
๐ SIMILAR VOLUMES
## Abstract This paper describes a method of using the vertical wetโbulb potential temperature distribution in the warm sector of a depression to estimate the amount of precipitation which that depression will give at a later time. The actual results of applying this method to a number of depressio