This paper examines the response of the high latitude ionosphere- thermosphere system during two intense geomagnetic storms. For that, data taken by instruments on board Dynamic Explorer 2 taken at heights of the F2-layer are used. These results represent a comparison of simultaneous measurements of storm disturbances in gas composition, electron density and temperature in common local time sectors. Documented are an increase in electron temperature and a decrease in electron density; increases both in electron temperature and electron density; and the correlation between electron density decreases and increases in the ratio N2/O. It is noticed that the decrease in electron density is sometimes due to an increase in the molecular nitrogen d...
Storm effects at F1-layer heights (160–200 km) were analyzed for the first time using Millstone Hi...
This paper discusses the behavior of ionospheric parameters that were obtained from electron density...
In this paper, the ionospheric response of a high latitude station to some intense geomagnetic storm...
Neutral gas composition and ionospheric measurements taken by the Dynamic Explorer 2 satellite at F2...
Neutral gas composition and ionospheric measurements taken by the Dynamic Explorer 2 satellite at F2...
An investigation is made in order to analyze the role of neutral gas composition in the equatorial a...
Neutral gas density data (molecular nitrogen N2 and atomic oxygen O) between 310 and 330 km of altit...
On March 13, 1989 magnetic storm effects on the mid- and low-latitude ionosphere were investigated. ...
Neutral gas composition data (molecular nitrogen N2, atomic oxygen O and argon Ar) from the Dynamic ...
An investigation of the response of the mid-high, mid and low latitude critical frequency foF2 to th...
Disturbances produced by geomagnetic storms in the higher regions of the Earth's atmosphere, such as...
The UCL-Sheffield coupled thermosphere/ionosphere model has been used to assess the consequences of ...
During geomagnetic storm events, the highly variable solar wind energy input in the magnetosphere si...
606-616A study of the intense geomagnetic storm on 2-6 April 2004 has been carried out using ionosp...
The effect of geomagnetic storms on the mid-high latitude F2 region is studied. For that, foF2 data ...
Storm effects at F1-layer heights (160–200 km) were analyzed for the first time using Millstone Hi...
This paper discusses the behavior of ionospheric parameters that were obtained from electron density...
In this paper, the ionospheric response of a high latitude station to some intense geomagnetic storm...
Neutral gas composition and ionospheric measurements taken by the Dynamic Explorer 2 satellite at F2...
Neutral gas composition and ionospheric measurements taken by the Dynamic Explorer 2 satellite at F2...
An investigation is made in order to analyze the role of neutral gas composition in the equatorial a...
Neutral gas density data (molecular nitrogen N2 and atomic oxygen O) between 310 and 330 km of altit...
On March 13, 1989 magnetic storm effects on the mid- and low-latitude ionosphere were investigated. ...
Neutral gas composition data (molecular nitrogen N2, atomic oxygen O and argon Ar) from the Dynamic ...
An investigation of the response of the mid-high, mid and low latitude critical frequency foF2 to th...
Disturbances produced by geomagnetic storms in the higher regions of the Earth's atmosphere, such as...
The UCL-Sheffield coupled thermosphere/ionosphere model has been used to assess the consequences of ...
During geomagnetic storm events, the highly variable solar wind energy input in the magnetosphere si...
606-616A study of the intense geomagnetic storm on 2-6 April 2004 has been carried out using ionosp...
The effect of geomagnetic storms on the mid-high latitude F2 region is studied. For that, foF2 data ...
Storm effects at F1-layer heights (160–200 km) were analyzed for the first time using Millstone Hi...
This paper discusses the behavior of ionospheric parameters that were obtained from electron density...
In this paper, the ionospheric response of a high latitude station to some intense geomagnetic storm...