Ionospheric response to the partial solar eclipse of March 29, 2006, according to the observations at Nizhni Novgorod and Murmansk

The results of observations of the solar eclipse ionospheric effects on March 29, 2006, are presented. The observations were conducted using the partial reflection method near Nizhni Novgorod and the vertical sounding method at the automatic ionospheric station near Murmansk. It has been obtained th...

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Veröffentlicht in:Geomagnetism and aeronomy 2008-02, Vol.48 (1), p.98-103
Hauptverfasser: Belikovich, V. V., Vyakhirev, V. D., Kalinina, E. E., Tereshchenko, V. D., Chernyakov, S. M., Tereshchenko, V. A.
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container_end_page 103
container_issue 1
container_start_page 98
container_title Geomagnetism and aeronomy
container_volume 48
creator Belikovich, V. V.
Vyakhirev, V. D.
Kalinina, E. E.
Tereshchenko, V. D.
Chernyakov, S. M.
Tereshchenko, V. A.
description The results of observations of the solar eclipse ionospheric effects on March 29, 2006, are presented. The observations were conducted using the partial reflection method near Nizhni Novgorod and the vertical sounding method at the automatic ionospheric station near Murmansk. It has been obtained that the electron density at altitudes of 77 and 91 km decreases by a factor of more than 4; in this case the response of the ionosphere at an altitude of 91 km lags behind the eclipse maximum phase on the Earth by approximately 20 min. It has been established that the eclipse in the E and F 1 regions of the polar ionosphere causes a change in the electron density by 15–20%. The delay time of this effect varies from 12 to 24 min depending on the altitude. It has been registered that the reflection virtual altitude at altitudes of the ionospheric F region increases in Murmansk and Nizhni Novgorod.
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title Ionospheric response to the partial solar eclipse of March 29, 2006, according to the observations at Nizhni Novgorod and Murmansk
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