Currents and turbulence in and near mid-latitude sporadic <i>E</i>-layers caused by strong acoustic impulses

The generation of Hall and field-aligned currents in and in the vicinity of nighttime mid-latitude sporadic <i>E</i>-layers moving under the action of strong acoustic impulses of seismic, anthropogenic, or meteorological nature is considered in a model presented in this paper. The in...

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Main Authors: V. A. Liperovsky, C.-V. Meister, K. Schlegel, C. Haldoupis
Format: Article
Language:English
Published: Copernicus Publications 1997-06-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/15/767/1997/angeo-15-767-1997.pdf
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spelling doaj-a729d25f6d3f4da3aa80547a24c1d7952020-11-24T22:10:11ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761997-06-011576777310.1007/s00585-997-0767-xCurrents and turbulence in and near mid-latitude sporadic <i>E</i>-layers caused by strong acoustic impulsesV. A. Liperovsky0C.-V. Meister1K. Schlegel2C. Haldoupis3United Institute of Physics of the Earth Moscow, RussiaPlasma Physics Project of the Institute for Theoretical Physics and Astrophysics at Potsdam University, GermanyMax-Planck-Institute for Aeronomie, Katlenburg-Lindau, GermanyUniversity of Crete, Iracleon, GreeceThe generation of Hall and field-aligned currents in and in the vicinity of nighttime mid-latitude sporadic <i>E</i>-layers moving under the action of strong acoustic impulses of seismic, anthropogenic, or meteorological nature is considered in a model presented in this paper. The influence of the electrical polarization fields caused by charges at the horizontal edges of the sporadic layers and the finite conductivity of the external circuits are also taken into account. The theoretical model is applicable for ionospheric altitudes between 95 and 130 km. The estimates show that under certain conditions in a system with two sporadic <i>E</i>-layers, one of which is the current generator and the other is situated in the external circuit, the Farley-Buneman instability could be generated. On the other hand, observations show that Farley-Buneman waves are likely responsible for the infrequent echoes of mid-latitude 50-MHz backscatter with Doppler velocities near 300 m s<sup>–1</sup>. The possibility exists that the proposed current-generator model is at the origin of the observed mid-latitude Farley-Buneman waves.https://www.ann-geophys.net/15/767/1997/angeo-15-767-1997.pdf
collection DOAJ
language English
format Article
sources DOAJ
author V. A. Liperovsky
C.-V. Meister
K. Schlegel
C. Haldoupis
spellingShingle V. A. Liperovsky
C.-V. Meister
K. Schlegel
C. Haldoupis
Currents and turbulence in and near mid-latitude sporadic <i>E</i>-layers caused by strong acoustic impulses
Annales Geophysicae
author_facet V. A. Liperovsky
C.-V. Meister
K. Schlegel
C. Haldoupis
author_sort V. A. Liperovsky
title Currents and turbulence in and near mid-latitude sporadic <i>E</i>-layers caused by strong acoustic impulses
title_short Currents and turbulence in and near mid-latitude sporadic <i>E</i>-layers caused by strong acoustic impulses
title_full Currents and turbulence in and near mid-latitude sporadic <i>E</i>-layers caused by strong acoustic impulses
title_fullStr Currents and turbulence in and near mid-latitude sporadic <i>E</i>-layers caused by strong acoustic impulses
title_full_unstemmed Currents and turbulence in and near mid-latitude sporadic <i>E</i>-layers caused by strong acoustic impulses
title_sort currents and turbulence in and near mid-latitude sporadic <i>e</i>-layers caused by strong acoustic impulses
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 1997-06-01
description The generation of Hall and field-aligned currents in and in the vicinity of nighttime mid-latitude sporadic <i>E</i>-layers moving under the action of strong acoustic impulses of seismic, anthropogenic, or meteorological nature is considered in a model presented in this paper. The influence of the electrical polarization fields caused by charges at the horizontal edges of the sporadic layers and the finite conductivity of the external circuits are also taken into account. The theoretical model is applicable for ionospheric altitudes between 95 and 130 km. The estimates show that under certain conditions in a system with two sporadic <i>E</i>-layers, one of which is the current generator and the other is situated in the external circuit, the Farley-Buneman instability could be generated. On the other hand, observations show that Farley-Buneman waves are likely responsible for the infrequent echoes of mid-latitude 50-MHz backscatter with Doppler velocities near 300 m s<sup>–1</sup>. The possibility exists that the proposed current-generator model is at the origin of the observed mid-latitude Farley-Buneman waves.
url https://www.ann-geophys.net/15/767/1997/angeo-15-767-1997.pdf
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