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- W2012188530 abstract "1. The chief question discussed in this paper (§§ 6—12) is that of the free oscillations of an atmosphere whose temperature varies with the altitude ; and in particular the case of a uniform vertical temperature-gradient is studied in some detail. For consistency it is assumed that the expansions and contractions follow the adiabatic law. The problem is treated as a two-dimensional one, the space co-ordinates involved being horizontal and vertical; and the more definite conclusions arrived at relate to the case where the (horizontal) wave-length is somewhat large in comparison with the height of the atmosphere. The results are most easily interpreted when the temperature-gradient does not fall much below that characteristic of a state of convective equilibrium. The normal modes of oscillation then fall into well-defined types." @default.
- W2012188530 created "2016-06-24" @default.
- W2012188530 date "1911-02-15" @default.
- W2012188530 modified "2023-10-12" @default.
- W2012188530 title "On atmospheric oscillations" @default.
- W2012188530 doi "https://doi.org/10.1098/rspa.1911.0008" @default.
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