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

International audience 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 ?s pulses during elevation scans through horizontally uniform backscatter permitted the use of inversion techniq...

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Main Authors: Jackel, B. J., Moorcroft, D. R., Schlegel, K.
Other Authors: Department of Physics, University of Western Ontario (UWO), Max-Planck-Institut für Aeronomie (MPI Aeronomie), Max-Planck-Gesellschaft
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 1997
Subjects:
Online Access:https://hal.science/hal-00316177
https://hal.science/hal-00316177/document
https://hal.science/hal-00316177/file/angeo-15-54-1997.pdf
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spelling ftinsu:oai:HAL:hal-00316177v1 2023-11-12T04:16:37+01:00 Characteristics of very large aspect angle E-region coherent echoes at 933 MHz Jackel, B. J. Moorcroft, D. R. Schlegel, K. Department of Physics University of Western Ontario (UWO) Max-Planck-Institut für Aeronomie (MPI Aeronomie) Max-Planck-Gesellschaft 1997 https://hal.science/hal-00316177 https://hal.science/hal-00316177/document https://hal.science/hal-00316177/file/angeo-15-54-1997.pdf en eng HAL CCSD European Geosciences Union hal-00316177 https://hal.science/hal-00316177 https://hal.science/hal-00316177/document https://hal.science/hal-00316177/file/angeo-15-54-1997.pdf info:eu-repo/semantics/OpenAccess ISSN: 0992-7689 EISSN: 1432-0576 Annales Geophysicae https://hal.science/hal-00316177 Annales Geophysicae, 1997, 15 (1), pp.54-62 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 1997 ftinsu 2023-10-25T16:25:42Z International audience 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 ?s 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. Article in Journal/Newspaper EISCAT Sodankylä Tromsø Institut national des sciences de l'Univers: HAL-INSU Sodankylä ENVELOPE(26.600,26.600,67.417,67.417) Tromsø
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Jackel, B. J.
Moorcroft, D. R.
Schlegel, K.
Characteristics of very large aspect angle E-region coherent echoes at 933 MHz
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description International audience 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 ?s 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.
author2 Department of Physics
University of Western Ontario (UWO)
Max-Planck-Institut für Aeronomie (MPI Aeronomie)
Max-Planck-Gesellschaft
format Article in Journal/Newspaper
author Jackel, B. J.
Moorcroft, D. R.
Schlegel, K.
author_facet Jackel, B. J.
Moorcroft, D. R.
Schlegel, K.
author_sort Jackel, B. J.
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 HAL CCSD
publishDate 1997
url https://hal.science/hal-00316177
https://hal.science/hal-00316177/document
https://hal.science/hal-00316177/file/angeo-15-54-1997.pdf
long_lat ENVELOPE(26.600,26.600,67.417,67.417)
geographic Sodankylä
Tromsø
geographic_facet Sodankylä
Tromsø
genre EISCAT
Sodankylä
Tromsø
genre_facet EISCAT
Sodankylä
Tromsø
op_source ISSN: 0992-7689
EISSN: 1432-0576
Annales Geophysicae
https://hal.science/hal-00316177
Annales Geophysicae, 1997, 15 (1), pp.54-62
op_relation hal-00316177
https://hal.science/hal-00316177
https://hal.science/hal-00316177/document
https://hal.science/hal-00316177/file/angeo-15-54-1997.pdf
op_rights info:eu-repo/semantics/OpenAccess
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