We present a preliminary table of mean values of the F2 region bottomside parameters B0 (thickness parameter) and B1 (shape parameter) for the time interval 00.00 LT-23.00 LT. Data from vertical ionospheric soundings at Havana (23°N; 278°E; Dip 54.6°N; Modip 44.8°N) during wintertime and low solar activity (R12≈15) were used in the study. The diurnal variation of B0 shows higher values during nighttime than during daytime. The B1 parameter tends to be lower during nighttime than during daytime
Improved ionospheric modeling requires a better understanding of the relationship between ionospheri...
This paper presents the statistical analysis of the diurnal variations of the F layer at the equator...
Data from two ionospheric sounders each from the northern and southern hemisphere, are used for a st...
Modern digital ionosonde measurements at low–middle latitude station, New Delhi, India, are used to ...
In this study a comparison is made of the Utah State University Time-Dependent Ionospheric Model (TD...
This paper presents an analysis of the variability of ionospheric characteristics (f o F2, M(3000)F2...
High resolution electron density profiles (Ne) measured with the Arecibo (18.4 N, 66.7 W), Incoheren...
124-129This paper presents diurnal, seasonal and solar activity effects on the variability of ionos...
The total electron content (TEC) of the ionosphere is a parameter often used to check the validity o...
240-250In the present work, ionospheric electron content (IEC) as well as critical frequency of F2 ...
High resolution electron density profiles (Ne) measured with the Arecibo (18.4 N, 66.7 W), Incoh...
Diurnal, seasonal and annual foF2 variability and the response of the F2-layer height over Jicamarca...
International audienceIn this paper, we report on the night-time equatorial F-layer height behaviour...
The diurnal, seasonal, and solar activity variations of the bottomside ionospheric profile parameter...
It is evident that fluctuations in a standard ionospheric parameter, the minimum (virtual) height (...
Improved ionospheric modeling requires a better understanding of the relationship between ionospheri...
This paper presents the statistical analysis of the diurnal variations of the F layer at the equator...
Data from two ionospheric sounders each from the northern and southern hemisphere, are used for a st...
Modern digital ionosonde measurements at low–middle latitude station, New Delhi, India, are used to ...
In this study a comparison is made of the Utah State University Time-Dependent Ionospheric Model (TD...
This paper presents an analysis of the variability of ionospheric characteristics (f o F2, M(3000)F2...
High resolution electron density profiles (Ne) measured with the Arecibo (18.4 N, 66.7 W), Incoheren...
124-129This paper presents diurnal, seasonal and solar activity effects on the variability of ionos...
The total electron content (TEC) of the ionosphere is a parameter often used to check the validity o...
240-250In the present work, ionospheric electron content (IEC) as well as critical frequency of F2 ...
High resolution electron density profiles (Ne) measured with the Arecibo (18.4 N, 66.7 W), Incoh...
Diurnal, seasonal and annual foF2 variability and the response of the F2-layer height over Jicamarca...
International audienceIn this paper, we report on the night-time equatorial F-layer height behaviour...
The diurnal, seasonal, and solar activity variations of the bottomside ionospheric profile parameter...
It is evident that fluctuations in a standard ionospheric parameter, the minimum (virtual) height (...
Improved ionospheric modeling requires a better understanding of the relationship between ionospheri...
This paper presents the statistical analysis of the diurnal variations of the F layer at the equator...
Data from two ionospheric sounders each from the northern and southern hemisphere, are used for a st...