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Subauroral electric fields observed by the Freja satellite: A statistical study

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TLDR
In this article, the authors scan Freja electric field data for subauroral electric fields (SAEF) to enable a comprehensive study of the ionospheric signatures of such electric fields.
Abstract
Over 12 months of Freja electric field data have been scanned for subauroral electric fields (SAEF) to enable a comprehensive study of the ionospheric signatures of such electric fields. SAEF are encountered from 1800 to 0200 MLT in agreement with an earlier study. However, a large majority of the SAEF are encountered at a time slightly premidnight (2200 – 2300 MLT), with rather few occurrences before 2000 MLT and after 2400 MLT. Furthermore, the strength of the subauroral electric field is generally much larger for events close to 2200 MLT than for other events. The data confirm that SAEF occur during the substorm recovery phase but also show that SAEF occur earlier during recovery when located close to 2200 MLT than at other local times. The dependence on season and geomagnetic activity is studied, and it is found that the SAEF are more commonly observed at times of high activity when the subauroral electric fields are also generally stronger, except close to winter solstice, when strong electric fields are observed during low activity. The potentials associated with the SAEF and the relation to interplanetary magnetic field By are also studied. The observations are discussed in context with substorm-related field-aligned currents and the midlatitude trough, and we present evidence that support and refine one of the proposed production mechanisms.

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Average characteristics and activity dependence of the subauroral polarization stream

TL;DR: In this article, the authors examined the occurrence and characteristics of a persistent secondary westward convection peak which lies equatorward of the auroral two-cell convection, and identified the latitudinally broad and persistent subauroral polarization stream (SAPS) which spans the nightside from dusk to the early morning sector for all Kp greater than 4.
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Multisatellite observations of rapid subauroral ion drifts (SAID)

TL;DR: In this paper, the authors present the first conjugate observations of subauroral ion drifts (SAID) in the magnetosphere and ionosphere and coincident measurements by four ionospheric satellites.
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Stormtime coupling of the ring current, plasmasphere, and topside ionosphere: Electromagnetic and plasma disturbances

TL;DR: In this paper, the authors compare plasma and field disturbances observed in the ring current/plasmasphere overlap region and in the conjugate ionosphere during the magnetic storm of 5 June 1991, using data from the Combined Release and Radiation Effects Satellite (CRRES) flying in a geostationary transfer orbit and three satellites of the Defense Meteorological Satellite Program (DMSP) series in Sun-synchronous polar orbits.
References
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Journal ArticleDOI

Semiannual variation of geomagnetic activity

TL;DR: In this article, it was proposed that the semiannual variation in geomagnetic activity is caused by a semiannually variation in the effective southward component of the interplanetary field.
Journal ArticleDOI

Large‐scale characteristics of field‐aligned currents associated with substorms

TL;DR: In this paper, the authors determined the statistical features of field-aligned currents during a large number of substorms from the magnetic field observations acquired with the Triad satellite, including the following: (1) the large-scale regions of fieldaligned currents determined previously by the authors (Iijima and Potemra, 1976a) persist during all phases of sub-storm activity, namely, region 1, located near the poleward boundary of the fieldaligned current region, and region 2, positioned near the equatorward boundary.
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A statistical model of auroral ion precipitation

TL;DR: The average global characteristics of precipitating auroral ions were determined using the data from the SSJ/4 detectors on the F6 and F7 satellites of the Defense Meteorological Satellite Program (DMSP) as discussed by the authors.
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Rapid subauroral ion drifts observed by Atmosphere Explorer C

TL;DR: In this article, the authors investigated the rapid subauroral ion drift features using data obtained over a nearly five-year period from the ion RPA/drift meter on the Atmosphere Explorer-C.
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Effects of electric fields and other processes upon the nighttime high-latitude F layer

TL;DR: In this paper, the formation of the electron-density trough region which lies equatorward of the auroral oval was studied with a special emphasis on the formation formation of electron density trough region.
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