Published 1930
| public
Journal Article
Schallgeschwindigkeit und Temperatur in der Stratosphäre
- Creators
- Gutenberg, B.
- Frankfurt, A. M.
Chicago
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Abstract
The registrations of air waves confirm consequences drawn before from ear-observations. The results gained from the graphs show that the height in which velocity of sound and temperature begin to increase is not the same in all cases. Sometimes especially in winter and in spring it is as low as 20 kms. A simple method of calculation is given to find the sound-velocity in the stratosphere.
Additional Information
© 1930 Geest & Portig.Additional details
- Eprint ID
- 100511
- Resolver ID
- CaltechAUTHORS:20200103-142800343
- Created
-
2020-01-08Created from EPrint's datestamp field
- Updated
-
2020-01-08Created from EPrint's last_modified field
- Other Numbering System Name
- Balch Graduate School of the Geological Sciences
- Other Numbering System Identifier
- 54