On the inversion of O sup + ( sup 2 D minus sup 2 P) 7320 Angstrom twilight airglow observations: A method for recovering both the ionization frequency and the thermospheric oxygen atom densities
Journal Article
·
· Journal of Geophysical Research; (United States)
- Univ. of Michigan, Ann Arbor (USA)
- Univ. of Alabama, Huntsville (USA)
In this paper, the authors demonstrate that it is possible to invert twilight observations of the O{sup +}({sup 2}D{minus}{sup 2}P){minus}7320 {Angstrom} airglow emission to obtain information about both the thermospheric atomic oxygen densities and the unattenuated O{sup +}({sup 2}P) ionization frequency. The efficacy of the proposed approach, which relies upon making twilight observations in more than one viewing direction, is illustrated using a synthetic data set and an inversion algorithm based on a simple photochemical model. The results of this study show that day-to-day variations in the thermospheric oxygen atom densities may be monitored from the ground without requiring complementary measurements of the solar EUV flux. The study also shows that twilight observations may be used to monitor variations in the solar flux components that are responsible for O{sup +}({sup 2}P) production and EUV heating of the upper thermosphere.
- OSTI ID:
- 5312987
- Journal Information:
- Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 96:A1; ISSN 0148-0227; ISSN JGREA
- Country of Publication:
- United States
- Language:
- English
Similar Records
A method for the retrieval of atomic oxygen density and temperature profiles from ground-based measurements of the O sup + ( sup 2 D minus sup 2 P) 7320- angstrom twilight airglow
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Journal Article
·
Thu Jan 31 23:00:00 EST 1991
· Journal of Geophysical Research; (United States)
·
OSTI ID:5257915
Technique to retrieve solar EUV flux and neutral thermospheric O, O{sub 2}, N{sub 2} and temperature from airglow measurements
Conference
·
Fri Dec 30 23:00:00 EST 1994
·
OSTI ID:227952
Mid- and low-latitude model of thermospheric emissions. 1. O sup + ( sup 2 P) 7320 angstrom and N sub 2 (2P) 3,371 angstrom
Journal Article
·
Fri Nov 30 23:00:00 EST 1990
· Journal of Geophysical Research; (United States)
·
OSTI ID:5268673
Related Subjects
640200 -- Atmospheric Physics
640201* -- Atmospheric Physics-- Auroral
Ionospheric
& Magetospheric Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
AIRGLOW
ALGORITHMS
ATMOSPHERIC CHEMISTRY
CHEMICAL COMPOSITION
CHEMISTRY
DENSITY
EARTH ATMOSPHERE
ELEMENTS
EMISSION SPECTRA
IONIZATION
MATHEMATICAL LOGIC
MATHEMATICAL MODELS
NONMETALS
OXYGEN
PHOTOCHEMISTRY
PHYSICAL PROPERTIES
RADIATIONS
SOLAR RADIATION
SPECTRA
STELLAR RADIATION
THERMOSPHERE
VARIATIONS
640201* -- Atmospheric Physics-- Auroral
Ionospheric
& Magetospheric Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
AIRGLOW
ALGORITHMS
ATMOSPHERIC CHEMISTRY
CHEMICAL COMPOSITION
CHEMISTRY
DENSITY
EARTH ATMOSPHERE
ELEMENTS
EMISSION SPECTRA
IONIZATION
MATHEMATICAL LOGIC
MATHEMATICAL MODELS
NONMETALS
OXYGEN
PHOTOCHEMISTRY
PHYSICAL PROPERTIES
RADIATIONS
SOLAR RADIATION
SPECTRA
STELLAR RADIATION
THERMOSPHERE
VARIATIONS