Airglow observations of the OI 7774 A multiplet at Arecibo during a magnetic storm

Physics

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Airglow, Electron Density Profiles, Fine Structure, Magnetic Storms, Radar Scattering, Geomagnetism, Mathematical Models, Neutral Particles, Oxygen Ions, Radio Telescopes, Thermosphere

Scientific paper

The paper considers airglow observations of the OI 7774 A multiplet observed during a geomagnetic storm. Theoretical calculations using electron density profiles obtained with the incoherent scatter radar show that the measured intensities cannot be explained by either radiative or ion-ion recombination reactions. A possible correlation between the airglow enhancement and D(st) was found; excitation by heavy neutral atoms or ions precipitating into the thermosphere is proposed as a possible explanation for enhanced 7774 A emission during this magnetic storm.

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