Free Oscillations of an Atmosphere in Which Temperature Increases Linearly With Height
Description:
Note presenting the concept that when the temperature in the atmosphere increases linearly with height, the speed of propagation of long waves does not approach a limit with increasing wave length, as in the case of an atmosphere in which the temperature at great heights is assumed to be constant or decreasing, but increases linearly with the period.
Date:
October 1950
Creator:
Pekeris, C. L.
Item Type:
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Partner:
UNT Libraries Government Documents Department