In this paper, we numerically estimate the nitric oxide density in auroras, using photometric data on 427.8, 557.7, and 630.0 nm emission intensities. The data were obtained at midnight at observatories of the Polar Geophysical Institute. These estimates were made using a numerical modeling procedure with a time-dependent model of the auroral ionosphere [Dashkevich et al., 2017]. It is shown that the NO density in the maximum of the altitude profile is between (1÷3.3)∙10^8 cm–3. The obtained estimates indicate the absence of a correlation between the [NO]max values and 427.8 nm emission intensities
On 14 July 1974 the Atmosphere Explorer-C satellite flew through an aurora at F-region altitudes jus...
peer reviewedA ratio phi/K of vertical nitric oxide flux to the eddy diffusion coefficient is derive...
Abstract. Measurements by the Student Nitric Oxide Explorer (SNOE) satellite ultraviolet spectromete...
High-latitude observations of fluorescent nitric oxide gamma bands were made before and during a str...
International audienceThe vibrational distribution of nitric oxide in the polar ionosphere computed ...
In December 2010 the last campaign of the German-Norwegian sounding rocket project ECOMA (Existence ...
International audienceVertical profiles of nitric oxide in the altitude range 90 to 105 km are deriv...
A time-dependent model of the auroral ionosphere including the odd nitrogen species, NO, N(D-2), and...
The incident particle flux ion and neutral composition data taken on the AE-D satellite have been us...
Nitric Oxide (NO) is produced by solar photolysis and auroral activity in the upper mesosphere and l...
We have performed a large statistical study of the peak emission altitude of green O(1D2–1S0) (557.7...
Nitric oxide (NO) is produced by solar photolysis and auroral activity in the upper mesosphere and l...
Abstract. A model of auroral electron deposition processes has been developed using Monte Carlo tech...
We have performed a large statistical study of the peak emission altitude of green O(1D2–1S0) (557.7...
Spectrometric measurements in normal aurora of O2+ first negative (1N) and N2+ first negative (1N) e...
On 14 July 1974 the Atmosphere Explorer-C satellite flew through an aurora at F-region altitudes jus...
peer reviewedA ratio phi/K of vertical nitric oxide flux to the eddy diffusion coefficient is derive...
Abstract. Measurements by the Student Nitric Oxide Explorer (SNOE) satellite ultraviolet spectromete...
High-latitude observations of fluorescent nitric oxide gamma bands were made before and during a str...
International audienceThe vibrational distribution of nitric oxide in the polar ionosphere computed ...
In December 2010 the last campaign of the German-Norwegian sounding rocket project ECOMA (Existence ...
International audienceVertical profiles of nitric oxide in the altitude range 90 to 105 km are deriv...
A time-dependent model of the auroral ionosphere including the odd nitrogen species, NO, N(D-2), and...
The incident particle flux ion and neutral composition data taken on the AE-D satellite have been us...
Nitric Oxide (NO) is produced by solar photolysis and auroral activity in the upper mesosphere and l...
We have performed a large statistical study of the peak emission altitude of green O(1D2–1S0) (557.7...
Nitric oxide (NO) is produced by solar photolysis and auroral activity in the upper mesosphere and l...
Abstract. A model of auroral electron deposition processes has been developed using Monte Carlo tech...
We have performed a large statistical study of the peak emission altitude of green O(1D2–1S0) (557.7...
Spectrometric measurements in normal aurora of O2+ first negative (1N) and N2+ first negative (1N) e...
On 14 July 1974 the Atmosphere Explorer-C satellite flew through an aurora at F-region altitudes jus...
peer reviewedA ratio phi/K of vertical nitric oxide flux to the eddy diffusion coefficient is derive...
Abstract. Measurements by the Student Nitric Oxide Explorer (SNOE) satellite ultraviolet spectromete...