## Abstract The humidity of the air was measured with a pressurized Dobson‐Brewer hygrometer in a Canberra aircraft up to heights of about 50,000 ft over southern England on 35 occasions during 1954. The frost point decreased with increasing height in the stratosphere and usually approached a const
Some further observations from aircraft of frost point and temperature up to 50,000 ft
✍ Scribed by N. C. Helliwell; J. K. Mackenzie; M. J. Kerley
- Publisher
- John Wiley and Sons
- Year
- 1957
- Tongue
- English
- Weight
- 304 KB
- Volume
- 83
- Category
- Article
- ISSN
- 0035-9009
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
During 1955, 46 measurements of frost point and temperature were made at varying altitudes up to about 50,000 ft using a Dobson‐Brewer pressurized frost‐point hygrometer and a flat‐plate thermometer mounted on the Canberra aircraft of the Meteorological Research Flight. The general character of these ascents in the lower stratosphere confirms the conclusions of earlier papers (Murgatroyd, Goldsmith and Hollings 1955). The mean frost point at 48,000 ft for the ascents made in 1954 and 1955 is ‐117°F and at 46,000 ft ‐115°F, with a standard deviation of about 3°F in each case.
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