Parallel electric fields produced by ionospheric injection

<p>It is well known that there exists a thin layer in the lower boundary of the ionosphere between altitudes of 80 and 140 km in which collisional ions and collisionless electrons mix. Local breakdown of charge neutrality may be initiated in this layer by electric fields from the magnetosphere...

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Main Author: O. Saka
Format: Article
Language:English
Published: Copernicus Publications 2023-09-01
Series:Annales Geophysicae
Online Access:https://angeo.copernicus.org/articles/41/369/2023/angeo-41-369-2023.pdf
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author O. Saka
author_facet O. Saka
author_sort O. Saka
collection DOAJ
description <p>It is well known that there exists a thin layer in the lower boundary of the ionosphere between altitudes of 80 and 140 km in which collisional ions and collisionless electrons mix. Local breakdown of charge neutrality may be initiated in this layer by electric fields from the magnetosphere as well as by electric fields generated there by the local neutral winds. The breakdown may be momentarily canceled by Pedersen currents, but complete neutralization is prevented because some ionospheric plasmas are released as outflows by parallel electric fields. Those parallel electric fields are produced by inherent plasma processes in the polar ionosphere and act as auroral drivers. A new scenario creating parallel potential gradients is proposed.</p>
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spelling doaj.art-55a41fd480594d8eb120e23f8ffd6b562023-09-19T09:36:32ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762023-09-014136937310.5194/angeo-41-369-2023Parallel electric fields produced by ionospheric injectionO. Saka<p>It is well known that there exists a thin layer in the lower boundary of the ionosphere between altitudes of 80 and 140 km in which collisional ions and collisionless electrons mix. Local breakdown of charge neutrality may be initiated in this layer by electric fields from the magnetosphere as well as by electric fields generated there by the local neutral winds. The breakdown may be momentarily canceled by Pedersen currents, but complete neutralization is prevented because some ionospheric plasmas are released as outflows by parallel electric fields. Those parallel electric fields are produced by inherent plasma processes in the polar ionosphere and act as auroral drivers. A new scenario creating parallel potential gradients is proposed.</p>https://angeo.copernicus.org/articles/41/369/2023/angeo-41-369-2023.pdf
spellingShingle O. Saka
Parallel electric fields produced by ionospheric injection
Annales Geophysicae
title Parallel electric fields produced by ionospheric injection
title_full Parallel electric fields produced by ionospheric injection
title_fullStr Parallel electric fields produced by ionospheric injection
title_full_unstemmed Parallel electric fields produced by ionospheric injection
title_short Parallel electric fields produced by ionospheric injection
title_sort parallel electric fields produced by ionospheric injection
url https://angeo.copernicus.org/articles/41/369/2023/angeo-41-369-2023.pdf
work_keys_str_mv AT osaka parallelelectricfieldsproducedbyionosphericinjection