Ultraviolet nightglow production near the magnetic equator by neutral particle precipitation

Physics

Scientific paper

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Equatorial Atmosphere, Magnetic Equator, Magnetic Storms, Neutral Particles, Nightglow, Particle Precipitation, Ion Recombination, Oxygen Spectra, Satellite-Borne Instruments, Ultraviolet Spectroscopy

Scientific paper

The near-midnight latitudinal (±45) distribution of the O I 911-Å, 1304-Å, and 1356-Å emissions, observed by the extreme ultraviolet (EUV) spectrometer on the STP 78-1 satellite, have been analyzed and compared as a function of geomagnetic activity. The dominant source of these emissions is radiative recombination of atomic oxygen ions; however, for geomagnetically disturbed periods, excess O I 1304-Å and 1356-Å emission is observed within ±5° of the dip equator. Neutral particle precipitation from the ring current is discussed as a possible source of the excess O I 1304-Å and 1356-Å emission.

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