Effects of neutral wind on the electron temperature at a height of 600 km in the low latitude region

Electron temperature observed by the Hinotori satellite with the low inclination at the height of ~600 km was studied in terms of local time, season, latitude, magnetic declination and solar flux intensity during a 16-month period from 1981 to 1982. The electron temperatures show steep rise in t...

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Main Authors: S. Watanabe, K.-I. Oyama
Format: Article
Language:English
Published: Copernicus Publications 1996-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/14/290/1996/angeo-14-290-1996.pdf
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author S. Watanabe
K.-I. Oyama
author_facet S. Watanabe
K.-I. Oyama
author_sort S. Watanabe
collection DOAJ
description Electron temperature observed by the Hinotori satellite with the low inclination at the height of ~600 km was studied in terms of local time, season, latitude, magnetic declination and solar flux intensity during a 16-month period from 1981 to 1982. The electron temperatures show steep rise in the early morning (well known as morning overshoot), decrease after that and again increase at ~18 hours (hereafter named as evening overshoot). Generally the morning overshoot becomes more enhanced in the winter hemisphere and for higher solar fluxes. The evening overshoot becomes more pronounced in the mid-latitude in all seasons and more enhanced in the winter hemisphere in the same way as the morning overshoot. A difference is seen between 210°–285° and 285°–360° longitudes where magnetic declination is different. The longitudinal dependence of electron temperature indicates that the neutral wind also contributes to the thermal structure in the low latitude ionosphere.
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spelling doaj.art-a104ed0e045d4456876208e8d3b106f92022-12-22T01:24:02ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761996-03-011429029610.1007/s00585-996-0290-5Effects of neutral wind on the electron temperature at a height of 600 km in the low latitude regionS. WatanabeK.-I. OyamaElectron temperature observed by the Hinotori satellite with the low inclination at the height of ~600 km was studied in terms of local time, season, latitude, magnetic declination and solar flux intensity during a 16-month period from 1981 to 1982. The electron temperatures show steep rise in the early morning (well known as morning overshoot), decrease after that and again increase at ~18 hours (hereafter named as evening overshoot). Generally the morning overshoot becomes more enhanced in the winter hemisphere and for higher solar fluxes. The evening overshoot becomes more pronounced in the mid-latitude in all seasons and more enhanced in the winter hemisphere in the same way as the morning overshoot. A difference is seen between 210°–285° and 285°–360° longitudes where magnetic declination is different. The longitudinal dependence of electron temperature indicates that the neutral wind also contributes to the thermal structure in the low latitude ionosphere.https://www.ann-geophys.net/14/290/1996/angeo-14-290-1996.pdf
spellingShingle S. Watanabe
K.-I. Oyama
Effects of neutral wind on the electron temperature at a height of 600 km in the low latitude region
Annales Geophysicae
title Effects of neutral wind on the electron temperature at a height of 600 km in the low latitude region
title_full Effects of neutral wind on the electron temperature at a height of 600 km in the low latitude region
title_fullStr Effects of neutral wind on the electron temperature at a height of 600 km in the low latitude region
title_full_unstemmed Effects of neutral wind on the electron temperature at a height of 600 km in the low latitude region
title_short Effects of neutral wind on the electron temperature at a height of 600 km in the low latitude region
title_sort effects of neutral wind on the electron temperature at a height of 600 km in the low latitude region
url https://www.ann-geophys.net/14/290/1996/angeo-14-290-1996.pdf
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