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Extreme enhancement in total electron content after sunset on 8 November 2004 and its connection with storm enhanced density

TLDR
In this paper, the ionospheric total electron content (TEC) was observed to have anomalously increased following a severe daytime positive TEC storm at longitudes of Japan.
Abstract
[1] After sunset on 8 November 2004, the ionospheric total electron content (TEC) was observed to have anomalously increased following a severe daytime positive TEC storm at longitudes of Japan. The observation was made using a dense GPS receiver network, and covered a geographic latitudinal range of 27 to 45°N. There was a greater increase in TEC at higher latitudes in the evening, and the TEC reached 90 TEC units at 45°N (∼40°N magnetic latitude) at 1145 UT (2045 LT). The TEC enhancement exhibited features significantly different from those of positive TEC storms normally observed at Japan's longitudes. These features are interpreted as low-latitude signatures of a storm enhanced density (SED). Previously, SEDs were reported only at longitudes of America, and this led to the hypothesis that geomagnetic field configurations at these longitudes play a role in their formation. The present observations indicate that SEDs can be observed at other longitudes.

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Penetration of high latitude electric fields effects tolow latitude during Sundial 1984

TL;DR: In this article, electric field penetration events were identified using F-region vertical-drift measurements obtained in the October 6-13, 1984 period by Jicamarcan incoherent-backscatter radar and corresponding h-prime F measurements from ionosondes at Fortaleza, Cachoeira Paulista, and Dakar.

Ionosphere and thermosphere: Derivation of TEC and estimation of instrumental biases from GEONET in Japan

TL;DR: In this paper, a method to derive the ionospheric total electron content (TEC) and to estimate the biases of GPS satellites and dual frequency receivers using the GPS Earth Observation Network (GEONET) in Japan is presented.
Journal ArticleDOI

Large magnetic storm-induced nighttime ionospheric flows at midlatitudes and their impacts on GPS-based navigation systems

TL;DR: In this paper, GPS phase fluctuations in conjunction with regional total electron content (TEC) maps, in situ measurements of subauroral polarization streams (SAPS) and auroral convection from several Defense Meteorological Satellite Program spacecraft, and dynasonde measurements at the Bear Lake Observatory obtained during the intense magnetic storm of 7-8 November 2004 have indicated the serious impact of large ionospheric velocities on GPS-based navigation systems within the midlatitude region in the North American sector.
Journal ArticleDOI

Solar proxies pertaining to empirical ionospheric total electron content models

TL;DR: In this paper, an artificial neural network (ANN) was used for predicting the ionospheric total electron content (TEC) as a target parameter by including new solar proxies/indices in the input space that were based on direct measurements of solar EUV/UV flux, SOHO_SEM26-34 (the integrated 26-34 nm EUV emission), and Mg II cwr (the core-to-wing ratio of Mg I 280 nm line), as well as the traditional indices F10.7 and R.
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Longitude sector comparisons of storm enhanced density

TL;DR: In this paper, an example of storm enhanced density (SED) formation over Russia and Northern Europe is presented, which persisted 15-20 hours and was fixed in local time near noon over Europe and then later observed over the American sector.
References
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Journal ArticleDOI

The ionospheric disturbance dynamo

TL;DR: In this article, a numerical simulation study of the thermospheric winds produced by auroral heating during magnetic storms, and of their global dynamo effects, establishes the main features of the ionospheric disturbance dynamo.
Journal ArticleDOI

Response of the thermosphere and ionosphere to geomagnetic storms

TL;DR: In this paper, four numerical simulations have been performed, at equinox, using a coupled thermosphere-ionosphere model, to illustrate the response of the upper atmosphere to geomagnetic storms.
Journal ArticleDOI

Storm time plasma transport at middle and high latitudes

TL;DR: In this article, a snowplow effect occurs in which the convection cell continually encounters fresh corotating ionospheric plasma along its equatorward edge, producing a latitudinally narrow region of storm-enhanced plasma density (SED) and increased total electron content which is advected toward higher latitudes in the noon sector.
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