Negative phases at South-American stations during magnetic storms

Ionospheric data at three South-American stations (in low, mid and high latitudes) show negative phases in the high latitude location during magnetic storms. The negative phases in foF2 are caused by changes in the ratio between atomic and molecular concentrations of the neutral atmosphere.We find...

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Main Authors: P.G. Richards, M.A. Abdu, X.T. Pincheira, I.S. Batista
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México, Instituto de Geofísica 2000-03-01
Series:Geofísica Internacional
Subjects:
Online Access:http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2000/01/pincheira.pdf
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author P.G. Richards
M.A. Abdu
X.T. Pincheira
I.S. Batista
author_facet P.G. Richards
M.A. Abdu
X.T. Pincheira
I.S. Batista
author_sort P.G. Richards
collection DOAJ
description Ionospheric data at three South-American stations (in low, mid and high latitudes) show negative phases in the high latitude location during magnetic storms. The negative phases in foF2 are caused by changes in the ratio between atomic and molecular concentrations of the neutral atmosphere.We find that at high latitudes the negative phases are well explained by the [O]/[N2] rate changes. As the latitude decreases, as the wind influence on the F2 layer peak is dominant, the propagation of gravity waves can explain short-lived negative phases. In low latitudes, disturbed thermospheric winds can cause time delays in the normal pattern of foF2, creating alternating positive and negative phases.
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spelling doaj.art-cfedda143b7d40548e88e790687d10d02023-08-02T01:24:33ZengUniversidad Nacional Autónoma de México, Instituto de GeofísicaGeofísica Internacional0016-71692000-03-01391109115Negative phases at South-American stations during magnetic stormsP.G. RichardsM.A. AbduX.T. PincheiraI.S. BatistaIonospheric data at three South-American stations (in low, mid and high latitudes) show negative phases in the high latitude location during magnetic storms. The negative phases in foF2 are caused by changes in the ratio between atomic and molecular concentrations of the neutral atmosphere.We find that at high latitudes the negative phases are well explained by the [O]/[N2] rate changes. As the latitude decreases, as the wind influence on the F2 layer peak is dominant, the propagation of gravity waves can explain short-lived negative phases. In low latitudes, disturbed thermospheric winds can cause time delays in the normal pattern of foF2, creating alternating positive and negative phases.http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2000/01/pincheira.pdfIonospheremagnetic stormsnegative phases
spellingShingle P.G. Richards
M.A. Abdu
X.T. Pincheira
I.S. Batista
Negative phases at South-American stations during magnetic storms
Geofísica Internacional
Ionosphere
magnetic storms
negative phases
title Negative phases at South-American stations during magnetic storms
title_full Negative phases at South-American stations during magnetic storms
title_fullStr Negative phases at South-American stations during magnetic storms
title_full_unstemmed Negative phases at South-American stations during magnetic storms
title_short Negative phases at South-American stations during magnetic storms
title_sort negative phases at south american stations during magnetic storms
topic Ionosphere
magnetic storms
negative phases
url http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2000/01/pincheira.pdf
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AT isbatista negativephasesatsouthamericanstationsduringmagneticstorms