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- W1967732819 startingPage "6868" @default.
- W1967732819 abstract "Theoretical calculations of the behavior of the solar semidiurnal tide (as excited by insolation absorbed by ozone and water vapor) in the thermosphere are used to calculate the mean heating of the thermosphere caused by the dissipation of the tidal energy by molecular viscosity and conductivity. It is shown that exospheric temperatures of about 600–700°K can be maintained without EUV heating." @default.
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- W1967732819 date "1970-11-20" @default.
- W1967732819 modified "2023-09-25" @default.
- W1967732819 title "Mean heating of the thermosphere by tides" @default.
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- W1967732819 doi "https://doi.org/10.1029/jc075i033p06868" @default.
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