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9. Ionization and Energy Exchange Processes 1.Solar extreme ultraviolet (EUV) is the major source of energy input into the thermospheres/ionospheres in the solar system. 2. Electron precipitation contributes near the magnetic poles. > 90 nm causes dissociation (O 2 O+O) nm causes ionization 5.Energy losses (sinks), from the ionosphere’ point of view, are airglow and the heating of the neutral atmosphere (thermosphere) 6.Energy flow diagram in Fig. 9.1
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9.1 Absorption of Solar Radiation in the Thermosphere (1)
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9.1 Absorption of Solar Radiation in the Thermosphere (1a)
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9.1 Absorption of Solar Radiation in the Thermosphere (2)
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9.1 Absorption of Solar Radiation in the Thermosphere (2a)
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9.1 Absorption of Solar Radiation in the Thermosphere (3)
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9.1 Absorption of Solar Radiation in the Thermosphere (3b)
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9.3 Photoionization (1)
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9.3 Photoionization (1a)
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9.3 Photoionization (2)
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11.4 Ionospheric Layers
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11.4 Ionospheric Layers (2)
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11.4 Ionospheric Layers (3)
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11.4 Ionospheric Layers (4)
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