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Background concentrations of photochemically active trace constituents in the stratosphere and upper troposphere

✍ Scribed by Lewis D. Kaplan


Publisher
Springer
Year
1973
Tongue
English
Weight
273 KB
Volume
106-108
Category
Article
ISSN
0033-4533

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## 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