Ion-acoustic solitary waves and spectrally uniform scattering cross section enhancements

Spectra measured by incoherent scatter radars are formed predominantly by scattering of the incident signal off ion-acoustic and Langmuir waves in the ionosphere. Occasionally, the upshifted and/or downshifted lines produced by the ion-acoustic waves are enhanced well above thermal levels and ref...

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Main Authors: J. Ekeberg, G. Wannberg, L. Eliasson, K. Stasiewicz
Format: Article
Language:English
Published: Copernicus Publications 2010-06-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/28/1299/2010/angeo-28-1299-2010.pdf
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spelling doaj-cc2fc75f0aef4bf4a3eb4c868452d8712020-11-24T22:58:34ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762010-06-01281299130610.5194/angeo-28-1299-2010Ion-acoustic solitary waves and spectrally uniform scattering cross section enhancementsJ. Ekeberg0G. Wannberg1L. Eliasson2K. Stasiewicz3K. Stasiewicz4Swedish Institute of Space Physics, Kiruna, SwedenSwedish Institute of Space Physics, Kiruna, SwedenSwedish Institute of Space Physics, Kiruna, SwedenSwedish Institute of Space Physics, Uppsala, SwedenSpace Research Centre, Polish Academy of Sciences, Warsaw, PolandSpectra measured by incoherent scatter radars are formed predominantly by scattering of the incident signal off ion-acoustic and Langmuir waves in the ionosphere. Occasionally, the upshifted and/or downshifted lines produced by the ion-acoustic waves are enhanced well above thermal levels and referred to as naturally enhanced ion-acoustic lines. In this paper, we study another kind of enhancement, which is spectrally uniform over the whole ion-line, i.e. the up- and downshifted shoulder and the spectral valley in between. Based on observations made with the EISCAT Svalbard radar (ESR) facility, we investigate the transient and spectrally uniform power enhancements, which can be explained by ion-acoustic solitary waves. We use a theory of nonlinear waves in a magnetized plasma to determine the properties of such waves and evaluate their effects on scattered signals measured by ESR. We suggest a new mechanism that can explain backscattered power enhancements by one order of magnitude above the thermal level and show that it is consistent with observations.https://www.ann-geophys.net/28/1299/2010/angeo-28-1299-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Ekeberg
G. Wannberg
L. Eliasson
K. Stasiewicz
K. Stasiewicz
spellingShingle J. Ekeberg
G. Wannberg
L. Eliasson
K. Stasiewicz
K. Stasiewicz
Ion-acoustic solitary waves and spectrally uniform scattering cross section enhancements
Annales Geophysicae
author_facet J. Ekeberg
G. Wannberg
L. Eliasson
K. Stasiewicz
K. Stasiewicz
author_sort J. Ekeberg
title Ion-acoustic solitary waves and spectrally uniform scattering cross section enhancements
title_short Ion-acoustic solitary waves and spectrally uniform scattering cross section enhancements
title_full Ion-acoustic solitary waves and spectrally uniform scattering cross section enhancements
title_fullStr Ion-acoustic solitary waves and spectrally uniform scattering cross section enhancements
title_full_unstemmed Ion-acoustic solitary waves and spectrally uniform scattering cross section enhancements
title_sort ion-acoustic solitary waves and spectrally uniform scattering cross section enhancements
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2010-06-01
description Spectra measured by incoherent scatter radars are formed predominantly by scattering of the incident signal off ion-acoustic and Langmuir waves in the ionosphere. Occasionally, the upshifted and/or downshifted lines produced by the ion-acoustic waves are enhanced well above thermal levels and referred to as naturally enhanced ion-acoustic lines. In this paper, we study another kind of enhancement, which is spectrally uniform over the whole ion-line, i.e. the up- and downshifted shoulder and the spectral valley in between. Based on observations made with the EISCAT Svalbard radar (ESR) facility, we investigate the transient and spectrally uniform power enhancements, which can be explained by ion-acoustic solitary waves. We use a theory of nonlinear waves in a magnetized plasma to determine the properties of such waves and evaluate their effects on scattered signals measured by ESR. We suggest a new mechanism that can explain backscattered power enhancements by one order of magnitude above the thermal level and show that it is consistent with observations.
url https://www.ann-geophys.net/28/1299/2010/angeo-28-1299-2010.pdf
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AT gwannberg ionacousticsolitarywavesandspectrallyuniformscatteringcrosssectionenhancements
AT leliasson ionacousticsolitarywavesandspectrallyuniformscatteringcrosssectionenhancements
AT kstasiewicz ionacousticsolitarywavesandspectrallyuniformscatteringcrosssectionenhancements
AT kstasiewicz ionacousticsolitarywavesandspectrallyuniformscatteringcrosssectionenhancements
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