Results 51 to 60 of about 1,267 (222)
Equatorial Electrojet & Interplanetary Plasma Parameters [PDF]
132-137A comparative study of the day-to-day changes of equatorial electrojet parameters and interplanetary plasma parameters indicates that the normal noon-time electrojet weakens and counter-electrojet intensifies when positive B∞ (towards sun ...
Kane, R. P.
core
Westward equatorial electrojet during daytime hours
The phenomenon of the depression of the geomagnetic horizontal field during the daytime hours of magnetically quiet days at equatorial stations is described.
Rastogi, R. G.
core +1 more source
Typical disturbances of the daytime equatorial F region observed with a high-resolution HF radar [PDF]
HF radar measurements were performed near the magnetic equator in Africa (Korhogo 9°24'63''N–5°37'38''W) during the International Equatorial Electrojet Year (1993–1994). The HF radar is a high-resolution zenithal radar.
E. Blanc, E. Houngninou
doaj +1 more source
Abstract The Madden–Julian Oscillation (MJO), a recurring intraseasonal (30–96 days) disturbance in the troposphere, strongly influences the E‐region and F‐region ionosphere through its modulation of atmospheric tides. Among these, the diurnal eastward wave number 3 (DE3) tide, driven by MJO‐modulated latent heating, carries MJO signals upward into the
Deepali Aggarwal +4 more
wiley +1 more source
Distortions in the height structure of the equatorial electrojet during counter electrojet events
This paper presents simultaneous observations made near the magnetic equator during counter electrojet events using a coherent VHF backscattcr radar, magnetometer and digital ionosonde to understand the physical processes that generate the counter ...
Subbarao, K. S. V. +3 more
core +1 more source
Abstract We present the first comprehensive multi‐instrument climatological study of quiet‐time equatorial F‐region vertical plasma drifts across South America, a region where the magnetic declination angle varies significantly. Our analysis of well‐established long‐term ground‐based data sets from the Jicamarca incoherent scatter radar spanning 1968 ...
Sophia R. Laranja +6 more
wiley +1 more source
Equatorial F-region during Counter-electrojet [PDF]
1-5The bottom side electron density profiles on two strong counter-electro days (27 and 28 Nov. 1967) are studied from the quarter-hoirly ionograms at an equatorial station, Kosikanal (sip 3.4oN). The typical equatorial noon bite-out in maximum F2-region
Sethia, G +3 more
core
Abstract The substorm current wedge constitutes the backbone of the substorm current system. Its field‐aligned current components include an upward current in the premidnight sector and a downward current in the midnight‐morning sector, which connect the auroral ionosphere to the magnetotail.
Tsugunobu Nagai, Iku Shinohara
wiley +1 more source
We present the observations of field‐aligned currents and the equatorial electrojet during the 23 March 2023 magnetic storm, focusing on the effect of the drastic decrease of the solar wind dynamic pressure occurred during the main phase.
Guan Le +6 more
doaj +1 more source
Investigation of the response time of the equatorial ionosphere in context of the equatorial electrojet and equatorial ionization anomaly [PDF]
Equatorial Electrojet (EEJ) and Equatorial Ionization Anomaly (EIA) are two large-scale processes in the equatorial/low latitude ionosphere, driven primarily by the eastward electric field during daytime.
L. Jose +4 more
doaj +1 more source

