Imaging radar observations of Farley Buneman waves during the JOULE II experiment

Vector electric fields and associated <I><B>E</B></I>&times;<I><B>B</B></I> drifts measured by a sounding rocket in the auroral zone during the NASA JOULE II experiment in January 2007, are compared with coherent scatter spectra measured by a 30...

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Main Authors: D. L. Hysell, G. Michhue, M. F. Larsen, R. Pfaff, M. Nicolls, C. Heinselman, H. Bahcivan
Format: Article
Language:English
Published: Copernicus Publications 2008-07-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/1837/2008/angeo-26-1837-2008.pdf
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spelling doaj-6b06e539fbe14e6595eb859c54954d852020-11-24T23:59:03ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-07-01261837185010.5194/angeo-26-1837-2008Imaging radar observations of Farley Buneman waves during the JOULE II experimentD. L. Hysell0G. Michhue1M. F. Larsen2R. Pfaff3M. Nicolls4C. Heinselman5H. Bahcivan6Earth and Atmospheric Sciences, Cornell University, Ithaca, NY, USAEarth and Atmospheric Sciences, Cornell University, Ithaca, NY, USADepartment of Physics, Clemson University, Clemson, SC, USANASA Goddard Space Flight Center, Greenbelt, MD, USASRI International, Menlo Park, CA, USASRI International, Menlo Park, CA, USASRI International, Menlo Park, CA, USAVector electric fields and associated <I><B>E</B></I>&times;<I><B>B</B></I> drifts measured by a sounding rocket in the auroral zone during the NASA JOULE II experiment in January 2007, are compared with coherent scatter spectra measured by a 30 MHz radar imager in a common volume. Radar imaging permits precise collocation of the spectra with the background electric field. The Doppler shifts and spectral widths appear to be governed by the cosine and sine of the convection flow angle, respectively, and also proportional to the presumptive ion acoustic speed. The neutral wind also contributes to the Doppler shifts. These findings are consistent with those from the JOULE I experiment and also with recent numerical simulations of Farley Buneman waves and instabilities carried out by Oppenheim et al. (2008). Simple linear analysis of the waves offers some insights into the spectral moments. A formula relating the spectral width to the flow angle, ion acoustic speed, and other ionospheric parameters is derived.https://www.ann-geophys.net/26/1837/2008/angeo-26-1837-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. L. Hysell
G. Michhue
M. F. Larsen
R. Pfaff
M. Nicolls
C. Heinselman
H. Bahcivan
spellingShingle D. L. Hysell
G. Michhue
M. F. Larsen
R. Pfaff
M. Nicolls
C. Heinselman
H. Bahcivan
Imaging radar observations of Farley Buneman waves during the JOULE II experiment
Annales Geophysicae
author_facet D. L. Hysell
G. Michhue
M. F. Larsen
R. Pfaff
M. Nicolls
C. Heinselman
H. Bahcivan
author_sort D. L. Hysell
title Imaging radar observations of Farley Buneman waves during the JOULE II experiment
title_short Imaging radar observations of Farley Buneman waves during the JOULE II experiment
title_full Imaging radar observations of Farley Buneman waves during the JOULE II experiment
title_fullStr Imaging radar observations of Farley Buneman waves during the JOULE II experiment
title_full_unstemmed Imaging radar observations of Farley Buneman waves during the JOULE II experiment
title_sort imaging radar observations of farley buneman waves during the joule ii experiment
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2008-07-01
description Vector electric fields and associated <I><B>E</B></I>&times;<I><B>B</B></I> drifts measured by a sounding rocket in the auroral zone during the NASA JOULE II experiment in January 2007, are compared with coherent scatter spectra measured by a 30 MHz radar imager in a common volume. Radar imaging permits precise collocation of the spectra with the background electric field. The Doppler shifts and spectral widths appear to be governed by the cosine and sine of the convection flow angle, respectively, and also proportional to the presumptive ion acoustic speed. The neutral wind also contributes to the Doppler shifts. These findings are consistent with those from the JOULE I experiment and also with recent numerical simulations of Farley Buneman waves and instabilities carried out by Oppenheim et al. (2008). Simple linear analysis of the waves offers some insights into the spectral moments. A formula relating the spectral width to the flow angle, ion acoustic speed, and other ionospheric parameters is derived.
url https://www.ann-geophys.net/26/1837/2008/angeo-26-1837-2008.pdf
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