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A direct measurement of the humidity in the stratosphere using a cooled-vapour trap

✍ Scribed by F. R. Barclay; M. J. W. Elliott; P. Goldsmith; J. V. Jelley

Publisher
John Wiley and Sons
Year
1961
Tongue
English
Weight
166 KB
Volume
87
Category
Article
ISSN
0035-9009

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πŸ“œ SIMILAR VOLUMES

A direct measurement of the humidity in
A direct measurement of the humidity in the stratosphere using a cooled-vapour trap
✍ F. R. Barclay; M. J. W. Elliott; P. Goldsmith; J. V. Jelley πŸ“‚ Article πŸ“… 1960 πŸ› John Wiley and Sons 🌐 English βš– 395 KB

## Abstract A vapour trap designed for sampling the water vapour and carbon dioxide of the stratosphere is described. The results of one flight at about 27 km over south‐east England are given and discussed.

In situ water vapour measurement, and a
In situ water vapour measurement, and a case study of the drying mechanism of the tropical lower stratosphere
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## Abstract During an experiment performed in tropical regions, water vapour content was measured in the lower stratosphere, using long duration balloons. A set of profiles show a vertical structure consistent with what has been named the tape‐recorder effect. One of the results, when the balloon d

On the direct measurement of humidity mi
On the direct measurement of humidity mixing ratio and its fluctuations
✍ P. A. Sheppard; M. K. Elnesr πŸ“‚ Article πŸ“… 1951 πŸ› John Wiley and Sons 🌐 English βš– 261 KB

## Abstract An apparatus is described for the direct measurement of humidity mixing ratio. It is designed primarily for recording the turbulent fluctuations in the mixing ratio in the lower atmosphere, and is based on an electrical analogue of the wet‐bulb equation, using dry‐ and wet‐bulb thermoco

The amount of water vapour in the strato
The amount of water vapour in the stratosphere and upper troposphere
✍ D. Brunt; A. K. Kapur πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 367 KB

## Abstract It is shown that within the stratosphere the humidity mixing ratio should remain constant with height, and a simple formula is derived, by means of which the total water vapour content of the stratosphere can be derived. This formula indicates that the total is 0Β·62 times the amount whi