Results 21 to 30 of about 1,267 (222)

Electrodynamical response of the Indian low-mid latitude ionosphere to the very large solar flare of 28 October 2003 – a case study [PDF]

open access: yesAnnales Geophysicae, 2009
The electrodynamic effects on the low-mid latitude ionospheric region have been investigated using GPS (global positioning system) data, ionosonde data and ΔH values, during the very large solar flare (X17.2/4B) of 28 October 2003.
G. Manju   +4 more
doaj   +1 more source

Equatorial electrojet as part of the global circuit: a case-study from the IEEY [PDF]

open access: yesAnnales Geophysicae, 1998
Geomagnetic storm-time variations often occur coherently at high latitude and the day-side dip equator where they affect the normal eastward Sq field. This paper presents an analysis of ground magnetic field and ionospheric electrodynamic data related
A. T. Kobea   +7 more
doaj   +1 more source

Longitudinal, seasonal and solar cycle variation in lunar tide influence on the equatorial electrojet [PDF]

open access: yesAnnales Geophysicae, 2017
It has been well documented that the lunar tidal waves can modulate the ionospheric electrodynamics and create a visible influence on the equatorial electrojet (EEJ). The lunar tide influence gets intensified around noon, primarily during new and full
E. Yizengaw, B. A. Carter
doaj   +1 more source

A model equatorial electrojet [PDF]

open access: yesJournal of Geophysical Research, 1966
Cross-sectional profile determination of equatorial electrojet for various longitudes along dip equator using set of Gauss coefficients for earth's magnetic ...
Masahisa Sugiura, Joseph C. Cain
openaire   +1 more source

Spatial Development of Strong Storm-Induced Ionospheric Perturbations during 25–27 August 2018

open access: yesRemote Sensing, 2023
The 25–27 August 2018 geomagnetic storm was the third largest storm in the 24th solar cycle. It was a surprising space event that originated from low-level solar activity.
Wang Li   +4 more
doaj   +1 more source

Variabilities of mesospheric tides and equatorial electrojet strength during major stratospheric warming events [PDF]

open access: yesAnnales Geophysicae, 2009
The present study demonstrates the relationship between the high latitude northern hemispheric major sudden stratospheric warming (SSW) events and the reversal in the afternoon equatorial electrojet (EEJ), often called the counter-electrojet (CEJ ...
S. Sridharan   +2 more
doaj   +1 more source

The field of the equatorial electrojet from CHAMP data [PDF]

open access: yesAnnales Geophysicae, 2006
We apply a simple linear transform, the along-track second derivative, to four years of scalar and vectorial data from the CHAMP satellite. This transform, reminiscent of techniques used in the interpretation of aeromagnetic surveys, is applied either
J.-L. Le Mouël   +2 more
doaj   +1 more source

Secondary irregularities in the equatorial electrojet [PDF]

open access: yesJournal of Geophysical Research, 1967
Although the two-stream instability theory, discussed by Farley, has been quite successful in accounting for many observed features of the plasma-wave irregularities produced in the equatorial electrojet, increased equipmental sensitivity and improved experimental techniques of observing the power spectrum of radio echoes from the electrojet have ...
Robert Cohen, Kenneth L. Bowles
openaire   +1 more source

Variations of the peak positions in the longitudinal profile of noon-time equatorial electrojet

open access: yesEarth, Planets and Space, 2020
In this study, the seasonal variations of the EEJ longitudinal profiles were examined based on the full CHAMP satellite magnetic measurements from 2001 to 2010. A total of 7537 satellite noon-time passes across the magnetic dip-equator were analyzed.
Zié Tuo   +4 more
doaj   +1 more source

Equatorial electrojet at African longitudes: first results from magnetic measurements [PDF]

open access: yesAnnales Geophysicae, 1998
In the framework of the French participation in the International Equatorial Electrojet Year (IEEY), ten magnetotelluric stations were installed between November 1992 and November 1994 along a 1200-km-long meridian profile, between Lamto (latitude 6.2°
V. Doumouya   +4 more
doaj   +1 more source

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