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Rotational Speed of the Upper Atmosphere : an Increase with Height above 200 km

✍ Scribed by KING-HELE, D. G.; SCOTT, DIANA W.


Book ID
109657332
Publisher
Nature Publishing Group
Year
1967
Tongue
English
Weight
99 KB
Volume
215
Category
Article
ISSN
0028-0836

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The average, longterm behaviour of many parameters P of the Earth's atmosphere and ionosphere depends on the solar activity cycle. In many cases it can be roughly described by a linear approximation of the form P = P0(1 + kR), where for example, P is electron density of the ionosphere or stratospher