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VII.—The Dynamics of Cyclones and Anticyclones. Part III

Published online by Cambridge University Press:  15 September 2014

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Extract

In 1900 I communicated to this Society a paper on the above subject. Since that date a great deal of information has been obtained by means of free balloons carrying instruments which recorded the temperature, humidity, and pressure of the air up to great elevations. Much of this new knowledge seems to contradict our previous ideas, and does not seem to fit into the old convectional theory that cyclones are formed by the rising of the hot, moist air from the surface of the earth; their energy being due to their temperature and to the heat liberated by the condensation of the water vapour in them. We are told by those who have studied the bearing of the new knowledge on our atmospheric circulation that the old theory is “utterly untenable.” Their reasons for this conclusion are, first, that the recent investigations show that the air is colder in cyclones than in anticyclones; second, that the isothermal layer is lower than the mean over cyclones, while it is higher than the mean over anticyclones. At first sight these discoveries seem to shatter the convectional theory, but before we come to any conclusion I should like to present certain facts which it appears to me will require to be considered before we scrap our old ideas.

Type
Proceedings
Copyright
Copyright © Royal Society of Edinburgh 1916

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References

page 174 note 1 Trans. Roy. Soc. Edin., vol. xl, part i (No. 7).

page 180 note * This experiment was shown at the meeting.

page 181 note * Trans. Roy. Soc. Edin., vol. xl, part i (No. 7).