On Continuous Observations of Thin Walls of High-Density Plasma in the High-Latitude Ionosphere from Arktika-M Satellites


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A new structure element of the Arctic ionosphere has been detected from the data of topside sounding of the ionosphere: quasi-vertical walls of high-density plasma. The importance of studying this phenomenon for geophysics and the practice of radio wave propagation in high latitudes is noted. The Arktika-M hydrometeorological space complex with an onboard ionosonde is proposed for its study. The possibility of observing and analyzing all life-cycle phases of this ionospheric inhomogeneity is shown.

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N. Danilkin

Fedorov Institute of Applied Geophysics

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Email: nickdanilkin88@yandex.ru
俄罗斯联邦, Moscow, 129128

G. Zhbankov

Southern Federal University

Email: nickdanilkin88@yandex.ru
俄罗斯联邦, Rostov-on-Don, 344006

V. Lapshin

Fedorov Institute of Applied Geophysics

Email: nickdanilkin88@yandex.ru
俄罗斯联邦, Moscow, 129128

M. Filippov

Fedorov Institute of Applied Geophysics

Email: nickdanilkin88@yandex.ru
俄罗斯联邦, Moscow, 129128

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