Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results

The implementation of a technique to derive mesospheric winds from HF radar observations of meteor echoes at Halley (76°S, 27°W), Antarctica, is described. The meteor echoes are observed at near ranges (less than 400 km) and have characteristics distinctly different from echoes backscattered from pl...

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Published in:Radio Science
Main Authors: Jenkins, B., Jarvis, M. J., Forbes, D. M.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 1998
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/504097/
https://doi.org/10.1029/98RS01113
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spelling ftnerc:oai:nora.nerc.ac.uk:504097 2023-05-15T13:48:08+02:00 Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results Jenkins, B. Jarvis, M. J. Forbes, D. M. 1998 http://nora.nerc.ac.uk/id/eprint/504097/ https://doi.org/10.1029/98RS01113 unknown American Geophysical Union Jenkins, B.; Jarvis, M. J.; Forbes, D. M. 1998 Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results. Radio Science, 33 (4). 957-965. https://doi.org/10.1029/98RS01113 <https://doi.org/10.1029/98RS01113> Publication - Article PeerReviewed 1998 ftnerc https://doi.org/10.1029/98RS01113 2023-02-04T19:38:15Z The implementation of a technique to derive mesospheric winds from HF radar observations of meteor echoes at Halley (76°S, 27°W), Antarctica, is described. The meteor echoes are observed at near ranges (less than 400 km) and have characteristics distinctly different from echoes backscattered from plasma irregularities in the E and F regions of the ionosphere. A Lorentzian model is used to fit the echo spectrum. The echo occurrence rate has the diurnal variation expected of meteors with a minimum in the afternoon. There also appears to be an annual variation which may be related to seasonal changes in the atmosphere. At present, results are confined to a single beam; that directed toward the south geographic pole is presented here, as this will give the meridional component of the wind and can be compared with other studies. The meridional wind is found to be dominated by the semidiurnal tide most of the year, with maxima in spring and autumn. Data for May 1996 show that the semidiurnal tide is dominant, but there are significant contributions from the 24-hour and 8-hour tides. A moving window spectral analysis technique allows the temporal behavior of the waves over a 10-day period to be studied. A quasi 2-day wave is observed during this interval, and slight changes of period with time can be observed. Planetary waves with periods of 5 and 10 days are observed during the winter of 1996. The radar has been operating since 1988, and so these data form a substantial and valuable database of mesospheric observations in the high-latitude southern hemisphere. Article in Journal/Newspaper Antarc* Antarctica W. Antarctica Natural Environment Research Council: NERC Open Research Archive Radio Science 33 4 957 965
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
description The implementation of a technique to derive mesospheric winds from HF radar observations of meteor echoes at Halley (76°S, 27°W), Antarctica, is described. The meteor echoes are observed at near ranges (less than 400 km) and have characteristics distinctly different from echoes backscattered from plasma irregularities in the E and F regions of the ionosphere. A Lorentzian model is used to fit the echo spectrum. The echo occurrence rate has the diurnal variation expected of meteors with a minimum in the afternoon. There also appears to be an annual variation which may be related to seasonal changes in the atmosphere. At present, results are confined to a single beam; that directed toward the south geographic pole is presented here, as this will give the meridional component of the wind and can be compared with other studies. The meridional wind is found to be dominated by the semidiurnal tide most of the year, with maxima in spring and autumn. Data for May 1996 show that the semidiurnal tide is dominant, but there are significant contributions from the 24-hour and 8-hour tides. A moving window spectral analysis technique allows the temporal behavior of the waves over a 10-day period to be studied. A quasi 2-day wave is observed during this interval, and slight changes of period with time can be observed. Planetary waves with periods of 5 and 10 days are observed during the winter of 1996. The radar has been operating since 1988, and so these data form a substantial and valuable database of mesospheric observations in the high-latitude southern hemisphere.
format Article in Journal/Newspaper
author Jenkins, B.
Jarvis, M. J.
Forbes, D. M.
spellingShingle Jenkins, B.
Jarvis, M. J.
Forbes, D. M.
Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results
author_facet Jenkins, B.
Jarvis, M. J.
Forbes, D. M.
author_sort Jenkins, B.
title Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results
title_short Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results
title_full Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results
title_fullStr Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results
title_full_unstemmed Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results
title_sort mesospheric wind observations derived from super dual auroral radar network (superdarn) hf radar meteor echoes at halley, antarctica: preliminary results
publisher American Geophysical Union
publishDate 1998
url http://nora.nerc.ac.uk/id/eprint/504097/
https://doi.org/10.1029/98RS01113
genre Antarc*
Antarctica
W. Antarctica
genre_facet Antarc*
Antarctica
W. Antarctica
op_relation Jenkins, B.; Jarvis, M. J.; Forbes, D. M. 1998 Mesospheric wind observations derived from Super Dual Auroral Radar Network (SuperDARN) HF radar meteor echoes at Halley, Antarctica: preliminary results. Radio Science, 33 (4). 957-965. https://doi.org/10.1029/98RS01113 <https://doi.org/10.1029/98RS01113>
op_doi https://doi.org/10.1029/98RS01113
container_title Radio Science
container_volume 33
container_issue 4
container_start_page 957
op_container_end_page 965
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