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• W2034949596 startingPage "1083" @default.
• W2034949596 abstract "A time-dependent model calculation of the interaction between energetic electrons and the thermosphere is performed to evaluate the heating efficiency. All energy channels which contribute to the neutral heating of the atmosphere are considered in detail. Neutral chemical reactions and deactivation of metastables are found to be the major heat sources. It is shown that, below 150km, the heating efficiency is on the order of 60% and nearly independent of altitude. At higher altitude, its value decreases in a manner depending on the atmosphere density and composition. It is concluded that, in the dayside polar cusp, particle heating may be an important source of thermospheric motion." @default.
• W2034949596 created "2016-06-24" @default.
• W2034949596 creator A5035139226 @default.
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• W2034949596 date "1982-11-01" @default.
• W2034949596 modified "2023-10-17" @default.
• W2034949596 title "The thermospheric heating efficiency under electron precipitation conditions" @default.
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• W2034949596 doi "https://doi.org/10.1016/0032-0633(82)90119-2" @default.
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