Diagnostics of emission intensities and electron density in auroras based on empirical precipitation models

Author:

Dashkevich Zhanna12,Ivanov Vladimir1

Affiliation:

1. Polar Geophysical Institute, RAS

2. Polar Geophysical Institute

Abstract

We have studied the influence of the precipitating electron spectrum shape on the integral intensity of emissions λ391.4 nm 1NG N⁺₂, λ670.4 mn 1PG N₂, λ337.1 nm 2PG N₂, λ320.0 nm VK N₂, λ127.3 nm LBH N₂, atomic oxygen emissions λ557.7 and λ630.0 nm, total electron content in the vertical column of aurora. The integral characteristics of the emission intensity and the total electron content are shown to weakly depend on the energy spectrum shape and to be determined mainly by average energy values Eev and energy flux value Fᴇ of precipitating electrons. An algorithm is proposed for diagnosing the planetary distribution of emission intensities and total electron content in auroras based on data from empirical electron precipitation models, without making a priori assumptions about the shape of the energy spectrum of precipitating electrons.

Publisher

Infra-M Academic Publishing House

Subject

Space and Planetary Science,Atmospheric Science,Geophysics

Reference14 articles.

1. Dashkevich Zh.V., Ivanov V.E., Sergienko T.I., Kozelov B.V. Physicochemical model of the auroral ionosphere.Cosmic Res. 2017, vol. 55, pp. 88–100. DOI: 10.1134/S0010952517020022., Dashkevich Zh.V., Ivanov V.E., Sergienko T.I., Kozelov B.V. Physicochemical model of the auroral ionosphere.Cosmic Res. 2017, vol. 55, pp. 88–100. DOI: 10.1134/S0010952517020022.

2. Dashkevich Zh.V., Ivanov V.E. The evaluation of efficiency O(1S) and O(1D) excitation mechanisms in aurora. Trudy Kolskogo nauchnogo tsentra RAN [Proc. Kola Scientific Center of the Russian Academy of Sciences]. 2018, vol. 5, pp. 69–75. (In Russian)., Dashkevich Zh.V., Ivanov V.E. The evaluation of efficiency O(1S) and O(1D) excitation mechanisms in aurora. Trudy Kolskogo nauchnogo tsentra RAN [Proc. Kola Scientific Center of the Russian Academy of Sciences]. 2018, vol. 5, pp. 69–75. (In Russian).

3. Ivanov V.E., Kozelov B.V. Prokhozhdenie elektronnykh i protonno-vodorodnykh puchkov v atmosphere Zemli [Transmission of electron and proton-hydrogen beams through Earth atmosphere]. Kola Scientific Center; Polar Geophysical Institute.Apatity, Kola Scientific Center Publ., 2001. 260 c., Ivanov V.E., Kozelov B.V. Prokhozhdenie elektronnykh i protonno-vodorodnykh puchkov v atmosphere Zemli [Transmission of electron and proton-hydrogen beams through Earth atmosphere]. Kola Scientific Center; Polar Geophysical Institute.Apatity, Kola Scientific Center Publ., 2001. 260 c.

4. Ivanov V.E., Kirillov A.S., Malkov M.V., Sergienko T.I., Starkov G.V. Boundaries of the aurora oval and the planetary model of the glow intensity. Geomagnetizm i aeronomiya. [Geomagnetism and Aeronomy]. 1993, vol. 33, pp. 80–88. (In Russian)., Ivanov V.E., Kirillov A.S., Malkov M.V., Sergienko T.I., Starkov G.V. Boundaries of the aurora oval and the planetary model of the glow intensity. Geomagnetizm i aeronomiya. [Geomagnetism and Aeronomy]. 1993, vol. 33, pp. 80–88. (In Russian).

5. Hardy D.A., Gussenhoven M.S., Holeman E. A statictical model of the auroral electron precipitation. J. Geophys. Res. 1985, vol. 90, pp. 4229–4248., Hardy D.A., Gussenhoven M.S., Holeman E. A statictical model of the auroral electron precipitation. J. Geophys. Res. 1985, vol. 90, pp. 4229–4248.

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