In order to understand the physics involved in the correlation between the equatorial electroject and magnetosphere-ionosphere coupling, the Senior-Blanc model is expanded for the condition involving the variation of the particle precipitation. A quasi-simulated calculation method is developed to study the potential distribution at middle and low latitudes and the equatorial electrojet when the boundaries or the driving potential changes abruptly. The results indicate a significant effect of the magnetosphere-ionosphere coupling on the equatorial electrojet. It shows that from early morning to midnight, an additional eastward electrojet occurs following the abrupt increase of the driving potential and equatorward expansion of the boundar...
A computer program which calculates electron and ion densities, ionospheric conductivities, electric...
The thermospheric neutral wind and ionospheric layer conductance at latitudes higher than 45 degrees...
Quiet-time daily variations of the geomagnetic field near the magnetic equator due to the equatorial...
The paper describes the consequences of the special features of the electric field and magnetic fiel...
Ground magnetic data of three low-latitude magnetic stations in China (Qiongzhong, Guangzhou and Qua...
The effects of large winds on the low-latitude E region ionosphere and the equatorial electrojet in ...
It has been known for a long time that the equatorial electrojet varies from day to day even when so...
Model calculations are used to analyse the function of the magnetosphere-ionosphere electro-dynamic ...
Topics discussed include equatorial electrojet and related phenomena, global ionosphere/thermosphere...
The paper is based on a detailed observational study of the Equatorial Spread F (ESF) events on geo...
It is shown that there are distinctly two different mechanisms for the interaction of solar wind wit...
Equatorial counterelectrojet (CEJ) events are analyzed in association with changes in the interplane...
Geomagnetic storm-time variations often occur coherently at high latitude and the day-side dip equa...
Abstract The determination of the physical parameters of the equatorial electrojet (EEJ) from Korhog...
In this work, a balance on the present status of the study of the equatorial electrojet is presented...
A computer program which calculates electron and ion densities, ionospheric conductivities, electric...
The thermospheric neutral wind and ionospheric layer conductance at latitudes higher than 45 degrees...
Quiet-time daily variations of the geomagnetic field near the magnetic equator due to the equatorial...
The paper describes the consequences of the special features of the electric field and magnetic fiel...
Ground magnetic data of three low-latitude magnetic stations in China (Qiongzhong, Guangzhou and Qua...
The effects of large winds on the low-latitude E region ionosphere and the equatorial electrojet in ...
It has been known for a long time that the equatorial electrojet varies from day to day even when so...
Model calculations are used to analyse the function of the magnetosphere-ionosphere electro-dynamic ...
Topics discussed include equatorial electrojet and related phenomena, global ionosphere/thermosphere...
The paper is based on a detailed observational study of the Equatorial Spread F (ESF) events on geo...
It is shown that there are distinctly two different mechanisms for the interaction of solar wind wit...
Equatorial counterelectrojet (CEJ) events are analyzed in association with changes in the interplane...
Geomagnetic storm-time variations often occur coherently at high latitude and the day-side dip equa...
Abstract The determination of the physical parameters of the equatorial electrojet (EEJ) from Korhog...
In this work, a balance on the present status of the study of the equatorial electrojet is presented...
A computer program which calculates electron and ion densities, ionospheric conductivities, electric...
The thermospheric neutral wind and ionospheric layer conductance at latitudes higher than 45 degrees...
Quiet-time daily variations of the geomagnetic field near the magnetic equator due to the equatorial...