67-74The paper describes the daily and seasonal variations of declination (or eastward geomagnetic field) at five equatorial electrojet observatories operating during 1958. The daily variation of declination in Central Asian sectors (Addis-Ababa and Trivandrum) showed a completely opposite character between the two solstices. The daily variation of declination at Huancayo showed a strong daytime peak during any of the seasons and at Jarvis during March and December. These abnormalities are suggested to be due to the different ionospheric electric conductivity profiles and due to complex dynamics caused by varying interaction between geographic and magnetic equators at different longitudes
International audienceHuancayo is the only equatorial electrojet station where the daytime increase ...
The structure of the equatorial electrojet during disturbed condition is examined using data from 10...
The paper examines the data of geographic northward (X), eastward (Y) and vertical (Z) components o...
The newly established geomagnetic field observations in Japan, have enabled us to analyse the 1998 d...
The yearly mean Disturbance Daily (SD) variation, i.e., solar daily variation on International Distu...
149-166The paper describes the diurnal and latitudinal variations of the horizontal (H), eastward (Y...
319-326The yearly average daily variation of the vertical component (Z) of geomagnetic field at the ...
With the establishment of the new geomagnetic field observations in the Ocean Hemisphere Network Pro...
Longitudinal, seasonal, and altitude-dependent variability of magnetic fields is investigated in equ...
Hourly values of the deviations in the geomagnetic X and Y field for the three years 1962-64 are stu...
The enhancement of the diurnal range of the horizontal component (H) of the earth's magnetic field o...
152-155Analysis of mean hourly values of H field from Trivandrum (dip 0.3°S) based on data derived f...
The paper discusses the variations of the horizontal (H), vertical (Z) and eastward (Y) components ...
The paper is based on a detailed observational study of the Equatorial Spread F (ESF) events on geo...
This paper discusses the effects of currents induced inside the Earth at equatorial latitudes due to...
International audienceHuancayo is the only equatorial electrojet station where the daytime increase ...
The structure of the equatorial electrojet during disturbed condition is examined using data from 10...
The paper examines the data of geographic northward (X), eastward (Y) and vertical (Z) components o...
The newly established geomagnetic field observations in Japan, have enabled us to analyse the 1998 d...
The yearly mean Disturbance Daily (SD) variation, i.e., solar daily variation on International Distu...
149-166The paper describes the diurnal and latitudinal variations of the horizontal (H), eastward (Y...
319-326The yearly average daily variation of the vertical component (Z) of geomagnetic field at the ...
With the establishment of the new geomagnetic field observations in the Ocean Hemisphere Network Pro...
Longitudinal, seasonal, and altitude-dependent variability of magnetic fields is investigated in equ...
Hourly values of the deviations in the geomagnetic X and Y field for the three years 1962-64 are stu...
The enhancement of the diurnal range of the horizontal component (H) of the earth's magnetic field o...
152-155Analysis of mean hourly values of H field from Trivandrum (dip 0.3°S) based on data derived f...
The paper discusses the variations of the horizontal (H), vertical (Z) and eastward (Y) components ...
The paper is based on a detailed observational study of the Equatorial Spread F (ESF) events on geo...
This paper discusses the effects of currents induced inside the Earth at equatorial latitudes due to...
International audienceHuancayo is the only equatorial electrojet station where the daytime increase ...
The structure of the equatorial electrojet during disturbed condition is examined using data from 10...
The paper examines the data of geographic northward (X), eastward (Y) and vertical (Z) components o...