Geomagnetic disturbances at F1-layer heights under different solar activity conditions over Norilsk

We analyze the influence of geomagnetic disturbances on the electron density Ne at Norilsk ionospheric station (69° N; 88° E) at F1-layer heights (120–200 km). For the analysis, we have selected 25 moderate and weak geomagnetic disturbances for two seasons — spring and fall — of 2003–2014. Using the...

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Bibliographic Details
Published in:Solar-Terrestrial Physics
Main Authors: Kushnarenko G.P., Yakovleva O.E., Kuznetsova G.M.
Format: Article in Journal/Newspaper
Language:English
Published: INFRA-M 2019
Subjects:
geomagnetic disturbances
electron density
spring-fall asymmetry
Astrophysics
QB460-466
Norilsk
norilsk
Online Access:https://doaj.org/article/cf0a503f5ace43d4b84e2819413f85c7
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Summary:We analyze the influence of geomagnetic disturbances on the electron density Ne at Norilsk ionospheric station (69° N; 88° E) at F1-layer heights (120–200 km). For the analysis, we have selected 25 moderate and weak geomagnetic disturbances for two seasons — spring and fall — of 2003–2014. Using the Ne values obtained from measurements made with the Norilsk digisonde during this period, we analyze Ne variations during geomagnetic disturbances in spring and fall for a long period of time. We determine the effect of spring-fall asymmetry occurring in all solar activity phases and manifesting itself in a significant decrease in the electron density during the main phase of fall storms at all heights in comparison with quiet days: up to 2.6 times at a height of 200 km and slightly less at lower heights. This phenomenon is not observed during spring disturbances: Ne variations are much weaker.

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