Abstract-- In this paper, we deal with the effect on the refractive index of seasonal anomaly in height of the ionospheric F2 peak for both, collisional and collisionless cases in the by using the real geometry of Earth’s magnetic field for north hemisphere. It is possible to say that there is an anti-symmetric harmony between the electron density and the all waves (for collisional and collisionless cases) at in hour when the seasonal anomaly occurs while there is an exact harmony in the real part of extra-ordinary wave (Z≠0)
Abstract. Annual and seasonal variations in the low-latitude topside ionosphere are investigated usi...
Annual and seasonal variations in the low-latitude topside ionosphere are investigated using observ...
Semiannual and annual variations in the F<SUB>2</SUB> region are examined by using f<SUB>o</SUB>F <S...
In this study, the seasonal behavior of the refractive index of the ionosphere over equator region i...
Newly published data on air pressures in the upper atmosphere suggest that seasonal variations of th...
For the first time, by using a regression procedure, we analyzed the solar activity dependence of th...
255-258Seasonal anomalies in the disturbed-day variations of f0F2 are described for the same station...
There are two different winter anomalies. A small one that appears in connection with ionization at ...
For the first time, by using a regression procedure, we analyzed the solar activity dependence of th...
The Winter Anomaly (WA) is an ionospheric phenomenon, particularly related to the F2-layer, that is ...
Data from two ionospheric sounders each from the northern and southern hemisphere, are used for a st...
A time-dependent, three-dimensional, multi-ion numerical model of the global ionosphere was used to ...
310-317The diurnal development of the equatorial anomaly is studied in two cases, viz. (i) the const...
219-223The winter anomaly in ionospheric absorption is studied at a mid-latitude station over half a...
In this study, the effect of the actual geometry of the magnetic field on the electron temperature h...
Abstract. Annual and seasonal variations in the low-latitude topside ionosphere are investigated usi...
Annual and seasonal variations in the low-latitude topside ionosphere are investigated using observ...
Semiannual and annual variations in the F<SUB>2</SUB> region are examined by using f<SUB>o</SUB>F <S...
In this study, the seasonal behavior of the refractive index of the ionosphere over equator region i...
Newly published data on air pressures in the upper atmosphere suggest that seasonal variations of th...
For the first time, by using a regression procedure, we analyzed the solar activity dependence of th...
255-258Seasonal anomalies in the disturbed-day variations of f0F2 are described for the same station...
There are two different winter anomalies. A small one that appears in connection with ionization at ...
For the first time, by using a regression procedure, we analyzed the solar activity dependence of th...
The Winter Anomaly (WA) is an ionospheric phenomenon, particularly related to the F2-layer, that is ...
Data from two ionospheric sounders each from the northern and southern hemisphere, are used for a st...
A time-dependent, three-dimensional, multi-ion numerical model of the global ionosphere was used to ...
310-317The diurnal development of the equatorial anomaly is studied in two cases, viz. (i) the const...
219-223The winter anomaly in ionospheric absorption is studied at a mid-latitude station over half a...
In this study, the effect of the actual geometry of the magnetic field on the electron temperature h...
Abstract. Annual and seasonal variations in the low-latitude topside ionosphere are investigated usi...
Annual and seasonal variations in the low-latitude topside ionosphere are investigated using observ...
Semiannual and annual variations in the F<SUB>2</SUB> region are examined by using f<SUB>o</SUB>F <S...