Physics
Scientific paper
Mar 2003
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30e..29s&link_type=abstract
Geophysical Research Letters, Volume 30, Issue 5, pp. 29-1, CiteID 1225, DOI 10.1029/2002GL015828
Physics
3
Ionosphere: Auroral Ionosphere (2704), Ionosphere: Particle Precipitation, Magnetospheric Physics: Magnetosphere/Ionosphere Interactions, Magnetospheric Physics: Energetic Particles, Precipitating
Scientific paper
All-sky spectral imagery has been used to study the altitude distribution of OII(732-733 nm), OI(630 nm), and N2(1PG) emissions in tall auroral rays appearing at the poleward edge of the auroral oval. The OII(732-733 nm) emission layer was consistently higher than the OI(630 nm) emission layer in these structures; the peak emission altitudes were estimated to be ~380 km and ~240 km, respectively. Neither the high absolute altitude of the OII(732-733 nm) peak nor its >100 km offset from the OI(630 nm) peak are consistent with published model results, which consider electron impact on atomic oxygen as the sole source of auroral O+(2P). The present results suggest that O+(2P) may also be excited directly from ambient ionospheric O+(4S) atoms. Other contributing factors may include a significant underestimation of the rate coefficients for O+(2P) quenching, or field-aligned up-flows of ionospheric O+.
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