Communication in Physical Sciences, 2021, 7(4): 542-553 Authors: Efiong A. Ibanga1* and Godwin A. Agbo2 Received: 25 July 2021/Accepted: 27 December 2021 The response of the ionosphere to heliophysical, interplanetary and geophysical structures during the severe geomagnetic storm (Dst=-223 nT) of March 17-18, 2015 has been investigated. Deviations of ordinary wave critical frequencies from the reference values based on four international geomagnetically quiet days preceding the storm (δfoF2) and F2 layer maximum electron density (NmF2) were calculated using manually scaled foF2 records from a chain of stations in Japan of the mid-latitude Asian sector. Results show that the pre-storm and main phases of the geomagnetic storm were...
International audienceThis study presents the longitudinal dependence of responses of the equatorial...
International audienceThis paper presents a study of the St Patrick's Day storm of 2015, with its io...
The ionospheric effects of six intense geomagnetic storms with Dst index ≤ −100 nT that occurred in ...
International audienceWe have presented a comparison between the modeled NmF2 and hmF2, and NmF2 and...
An investigation is made of the intense storms of April 12- 14, 1981(Dst =-311nT) in an attempt to c...
In this study, we documented the midlatitude F2-layer response to five strong geomagnetic storms wit...
The geomagnetic storm effects on the F2-region ionospheric parameters namely, foF2 (critical frequen...
The interaction of solar wind with earth's magnetic field leads to a number of modifications of the ...
606-616A study of the intense geomagnetic storm on 2-6 April 2004 has been carried out using ionosp...
International audienceIn this paper, the ionospheric quiet-time disturbances otherwise known as Pre-...
An investigation of the response of the mid-high, mid and low latitude critical frequency foF2 to th...
We have studied the ionospheric response at near-equator latitudes during the geomagnetic storm of 2...
A study is made of the intense storms of March 13–15, 1989 (Dst = –600nT), October 20–21, 1989 (Dst...
This study presents observed behavior of ionospheric responses using vertical total electron content...
Ionospheric response to geomagnetic storms is determined by the efficiency of the solar wind-magneto...
International audienceThis study presents the longitudinal dependence of responses of the equatorial...
International audienceThis paper presents a study of the St Patrick's Day storm of 2015, with its io...
The ionospheric effects of six intense geomagnetic storms with Dst index ≤ −100 nT that occurred in ...
International audienceWe have presented a comparison between the modeled NmF2 and hmF2, and NmF2 and...
An investigation is made of the intense storms of April 12- 14, 1981(Dst =-311nT) in an attempt to c...
In this study, we documented the midlatitude F2-layer response to five strong geomagnetic storms wit...
The geomagnetic storm effects on the F2-region ionospheric parameters namely, foF2 (critical frequen...
The interaction of solar wind with earth's magnetic field leads to a number of modifications of the ...
606-616A study of the intense geomagnetic storm on 2-6 April 2004 has been carried out using ionosp...
International audienceIn this paper, the ionospheric quiet-time disturbances otherwise known as Pre-...
An investigation of the response of the mid-high, mid and low latitude critical frequency foF2 to th...
We have studied the ionospheric response at near-equator latitudes during the geomagnetic storm of 2...
A study is made of the intense storms of March 13–15, 1989 (Dst = –600nT), October 20–21, 1989 (Dst...
This study presents observed behavior of ionospheric responses using vertical total electron content...
Ionospheric response to geomagnetic storms is determined by the efficiency of the solar wind-magneto...
International audienceThis study presents the longitudinal dependence of responses of the equatorial...
International audienceThis paper presents a study of the St Patrick's Day storm of 2015, with its io...
The ionospheric effects of six intense geomagnetic storms with Dst index ≤ −100 nT that occurred in ...