Plasma channels in the Venus upper ionosphere

The structure of the Venus nightside ionosphere is modeled in terms of a flow configuration derived from the position of the intermediate transition along the flanks of the ionosheath downstream from the magnetic polar regions. It is suggested that the shocked solar wind erodes more strongly the pol...

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Main Author: H. Pérez de Tejada
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México, Instituto de Geofísica 2001-05-01
Series:Geofísica Internacional
Subjects:
Online Access:http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2001/01/perez.pdf
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author H. Pérez de Tejada
author_facet H. Pérez de Tejada
author_sort H. Pérez de Tejada
collection DOAJ
description The structure of the Venus nightside ionosphere is modeled in terms of a flow configuration derived from the position of the intermediate transition along the flanks of the ionosheath downstream from the magnetic polar regions. It is suggested that the shocked solar wind erodes more strongly the polar ionosphere producing plasma channels that extend downstream from the magnetic polar regions. Such features represent the main source of mass loss along the plasma tail and imply a small overall solar wind-induced depletion of the planetary ionosphere. The plasma channels can account for the observation of ionospheric holes in PVO passes through the Venus wake. The expected flow distribution within the wake is consistent with the entry of plasma fluxes from the magnetic polar regions that was suggested earlier to account for geometry of the nightside ionopause (Pérez de Tejada, 1980).
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spelling doaj.art-4391f639fd2546a1acc718b40d5fed432023-09-02T21:47:06ZengUniversidad Nacional Autónoma de México, Instituto de GeofísicaGeofísica Internacional0016-71692001-05-014014352Plasma channels in the Venus upper ionosphereH. Pérez de TejadaThe structure of the Venus nightside ionosphere is modeled in terms of a flow configuration derived from the position of the intermediate transition along the flanks of the ionosheath downstream from the magnetic polar regions. It is suggested that the shocked solar wind erodes more strongly the polar ionosphere producing plasma channels that extend downstream from the magnetic polar regions. Such features represent the main source of mass loss along the plasma tail and imply a small overall solar wind-induced depletion of the planetary ionosphere. The plasma channels can account for the observation of ionospheric holes in PVO passes through the Venus wake. The expected flow distribution within the wake is consistent with the entry of plasma fluxes from the magnetic polar regions that was suggested earlier to account for geometry of the nightside ionopause (Pérez de Tejada, 1980).http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2001/01/perez.pdfVenus ionosphereplasma channelsionospheric holes
spellingShingle H. Pérez de Tejada
Plasma channels in the Venus upper ionosphere
Geofísica Internacional
Venus ionosphere
plasma channels
ionospheric holes
title Plasma channels in the Venus upper ionosphere
title_full Plasma channels in the Venus upper ionosphere
title_fullStr Plasma channels in the Venus upper ionosphere
title_full_unstemmed Plasma channels in the Venus upper ionosphere
title_short Plasma channels in the Venus upper ionosphere
title_sort plasma channels in the venus upper ionosphere
topic Venus ionosphere
plasma channels
ionospheric holes
url http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/2001/01/perez.pdf
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