Physics
Scientific paper
Oct 1986
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986jgr....9111365a&link_type=abstract
Journal of Geophysical Research (ISSN 0148-0227), vol. 91, Oct. 1, 1986, p. 11365-11368.
Physics
12
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.
Abreu Vincent J.
Chakrabarti Sangeeta
Eastes Richard Wayne
Solomon Stanley C.
Yee Jae Hyung
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