The structure of the Interplanetary Magnetic Field (IMF) is responsible for an essential part of the variability of the ionospheric plasma as demonstrated by investigations of the influence of IMF sector boundary crossings as well as of ?Bz-changes (defined from satellite observations) to the maximal electron density of the F2-layer at different stations in mid-latitudes. It could be shown that negative Bz-values cause distinct negative ionospheric effects. Maximal effects were detected at high geomagnetic latitudes (ionospheric response decreases with decreasing latitude), high solar/geomagnetic activity, equinoxes and night-time conditions
We examine the ionospheric F2-layer electron density variation by solar activity in middle latitude ...
An investigation of the response of the mid-high, mid and low latitude critical frequency foF2 to th...
606-616A study of the intense geomagnetic storm on 2-6 April 2004 has been carried out using ionosp...
The structure of the Interplanetary Magnetic Field (IMF) is responsible for an essential part of the...
Using critical frequencies, f0F2 from the Lannion, Slough, Poitiers, Garchy, Dourbes, Rome, Juliusru...
46-50The critical frequency of the ionosphere, apart from the diurnal and annual variations exhibit ...
Using criticaI frequencies, f0F2 from the Uppsala, Lannion and Dourbes ionosonde stations, the possi...
The possible effects of the orientation of the IMF on the ionosphere has been studied by Tulunay (19...
The Influence of the north–south component (Bz) of the interplanetary magnetic field (IMF) on geomag...
On March 13, 1989 magnetic storm effects on the mid- and low-latitude ionosphere were investigated. ...
A long-term trend in the F2-layer critical frequency (foF2) has been distinguished based on daytime ...
The Earth's magnetic field presents long-term variations with changes in strength and orientation. P...
As shown by ground-based absorption measurements, the lower ionospheric plasma is markedly controlle...
International audienceSuperposed epoch studies have been carried out in order to determine the ionos...
International audienceIn this work an attempt to identify the role of the interplanetary magnetic fi...
We examine the ionospheric F2-layer electron density variation by solar activity in middle latitude ...
An investigation of the response of the mid-high, mid and low latitude critical frequency foF2 to th...
606-616A study of the intense geomagnetic storm on 2-6 April 2004 has been carried out using ionosp...
The structure of the Interplanetary Magnetic Field (IMF) is responsible for an essential part of the...
Using critical frequencies, f0F2 from the Lannion, Slough, Poitiers, Garchy, Dourbes, Rome, Juliusru...
46-50The critical frequency of the ionosphere, apart from the diurnal and annual variations exhibit ...
Using criticaI frequencies, f0F2 from the Uppsala, Lannion and Dourbes ionosonde stations, the possi...
The possible effects of the orientation of the IMF on the ionosphere has been studied by Tulunay (19...
The Influence of the north–south component (Bz) of the interplanetary magnetic field (IMF) on geomag...
On March 13, 1989 magnetic storm effects on the mid- and low-latitude ionosphere were investigated. ...
A long-term trend in the F2-layer critical frequency (foF2) has been distinguished based on daytime ...
The Earth's magnetic field presents long-term variations with changes in strength and orientation. P...
As shown by ground-based absorption measurements, the lower ionospheric plasma is markedly controlle...
International audienceSuperposed epoch studies have been carried out in order to determine the ionos...
International audienceIn this work an attempt to identify the role of the interplanetary magnetic fi...
We examine the ionospheric F2-layer electron density variation by solar activity in middle latitude ...
An investigation of the response of the mid-high, mid and low latitude critical frequency foF2 to th...
606-616A study of the intense geomagnetic storm on 2-6 April 2004 has been carried out using ionosp...