Physics
Scientific paper
Jan 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001jgr...106..141l&link_type=abstract
Journal of Geophysical Research, Volume 106, Issue A1, p. 141-148
Physics
16
Atmospheric Composition And Structure: Airglow And Aurora, Atmospheric Composition And Structure: Thermosphere-Energy Deposition, Ionosphere: Particle Precipitation, Magnetospheric Physics: Auroral Phenomena
Scientific paper
A red aurora occurred over southern Canada and central Maine on April 11, 1997, producing a brightness of O I(630 nm) of several Kilorayleighs, which lasted for several hours. Two passes of the Defense Meteorological Satellite Program (DMSP) F12 satellite occurred during this time, and optical data were obtained from four CEDAR Optical Tomographic Imaging Facility (COTIF) sites. The DMSP F12 particle spectrometers observed proton precipitation south of the electron aurora with energy fluxes of several mW m-2. Tomographic inversion of the COTIF optical observations gives the altitude profile of emissions along a magnetic meridian. We combine all available data using an ionospheric auroral model. Our analysis shows that the model produces the observed auroral brightness from the proton precipitation alone.
Galand Marina
Lummerzheim Dirk
Mendillo Michael J.
Rees Manfred H.
Rich Frederic J.
No associations
LandOfFree
Emission of O I(630 nm) in proton aurora does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Emission of O I(630 nm) in proton aurora, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Emission of O I(630 nm) in proton aurora will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1363547