The ratio of OI 5577 A to N2(+) 3914 A under diffuse auroral condition

Details The ratio of OI 5577 A to N2(+) 3914 A under diffuse auroral condition The ratio of OI 5577 A to N2(+) 3914 A under diffuse auroral condition

Jan 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985chjss...5...34t&link_type=abstract

Chinese Journal of Space Sciences, vol. 5, Jan. 1985, p. 34-39. In Chinese, with abstract in English.

Physics

Atomic Physics

Auroral Spectroscopy, Nitrogen Ions, Oxygen Ions, Thermosphere, Altitude, Quenching (Atomic Physics), Ratios

Scientific paper

A linear relationship between the ratio OI 5577 A to N2(+) 3914 A and
the corresponding altitudes are found in this paper. With this
dependence the quenching factor of O(1S) in the lower thermosphere is
obtained; this quenching factor is not very large.

Affiliated with

Also associated with

No associations

Rating

The ratio of OI 5577 A to N2(+) 3914 A under diffuse auroral condition 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 The ratio of OI 5577 A to N2(+) 3914 A under diffuse auroral condition, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The ratio of OI 5577 A to N2(+) 3914 A under diffuse auroral condition will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-926190