Characteristics of very large aspect angle E-region coherent echoes at 933 MHz

The EISCAT UHF radar system was used to study the characteristics of E-region coherent backscatter at very large magnetic aspect angles (5–11°). Data taken using 60 μs pulses during elevation scans through horizontally uniform backscatter permitted the use of inversion techniques to d...

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Main Authors: B. J. Jackel, D. R. Moorcroft, K. Schlegel
Format: Article
Language:English
Published: Copernicus Publications 1997-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/15/54/1997/angeo-15-54-1997.pdf
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spelling doaj-5a0431be3e6a45d79191dfe1e9ebdf902020-11-24T22:59:56ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761997-01-0115546210.1007/s00585-997-0054-xCharacteristics of very large aspect angle E-region coherent echoes at 933 MHzB. J. Jackel0D. R. Moorcroft1K. Schlegel2Department of Physics, University of Western Ontario, London, Ontario, Canada, N6A 3K7Department of Physics, University of Western Ontario, London, Ontario, Canada, N6A 3K7Max-Plank-Institut für Aeronomie, Postfach 20, D-37189 Katlenburg-Lindau, Federal Republic of GermanyThe EISCAT UHF radar system was used to study the characteristics of E-region coherent backscatter at very large magnetic aspect angles (5–11°). Data taken using 60 μs pulses during elevation scans through horizontally uniform backscatter permitted the use of inversion techniques to determine height profiles of the scattering layer. The layer was always singly peaked, with a mean height of 104 km, and mean thickness (full width at half maximum) of 10 km, both independent of aspect angle. Aspect sensitivities were also estimated, with the Sodankylä-Tromsø link observing 5 dB/degree at aspect angles near 5°, decreasing to 3 dB/degree at 10° aspect angle. Observed coherent phase velocities from all three stations were found to be roughly consistent with LOS measurements of a common E-region phase velocity vector. The E-region phase velocity had the same orientation as the F-region ion drift velocity, but was approximately 50% smaller in magnitude. Spectra were narrow with skewness of about +1 (for negative velocities), increasing slightly with aspect angle.https://www.ann-geophys.net/15/54/1997/angeo-15-54-1997.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. J. Jackel
D. R. Moorcroft
K. Schlegel
spellingShingle B. J. Jackel
D. R. Moorcroft
K. Schlegel
Characteristics of very large aspect angle E-region coherent echoes at 933 MHz
Annales Geophysicae
author_facet B. J. Jackel
D. R. Moorcroft
K. Schlegel
author_sort B. J. Jackel
title Characteristics of very large aspect angle E-region coherent echoes at 933 MHz
title_short Characteristics of very large aspect angle E-region coherent echoes at 933 MHz
title_full Characteristics of very large aspect angle E-region coherent echoes at 933 MHz
title_fullStr Characteristics of very large aspect angle E-region coherent echoes at 933 MHz
title_full_unstemmed Characteristics of very large aspect angle E-region coherent echoes at 933 MHz
title_sort characteristics of very large aspect angle e-region coherent echoes at 933 mhz
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 1997-01-01
description The EISCAT UHF radar system was used to study the characteristics of E-region coherent backscatter at very large magnetic aspect angles (5–11°). Data taken using 60 μs pulses during elevation scans through horizontally uniform backscatter permitted the use of inversion techniques to determine height profiles of the scattering layer. The layer was always singly peaked, with a mean height of 104 km, and mean thickness (full width at half maximum) of 10 km, both independent of aspect angle. Aspect sensitivities were also estimated, with the Sodankylä-Tromsø link observing 5 dB/degree at aspect angles near 5°, decreasing to 3 dB/degree at 10° aspect angle. Observed coherent phase velocities from all three stations were found to be roughly consistent with LOS measurements of a common E-region phase velocity vector. The E-region phase velocity had the same orientation as the F-region ion drift velocity, but was approximately 50% smaller in magnitude. Spectra were narrow with skewness of about +1 (for negative velocities), increasing slightly with aspect angle.
url https://www.ann-geophys.net/15/54/1997/angeo-15-54-1997.pdf
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