Radar meteor decay rate variability and atmospheric consequences

The reasons for scatter in plots of log(inverse decay times) vs. height for radio meteor echoes are examined, and an explanation for the characteristics is offered. Effects like temperature variability, pressure variation, angular detection accuracy, pulse length, phase errors, plasma processes...

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Main Author: W. K. Hocking
Format: Article
Language:English
Published: Copernicus Publications 2004-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/3805/2004/angeo-22-3805-2004.pdf
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author W. K. Hocking
author_facet W. K. Hocking
author_sort W. K. Hocking
collection DOAJ
description The reasons for scatter in plots of log(inverse decay times) vs. height for radio meteor echoes are examined, and an explanation for the characteristics is offered. Effects like temperature variability, pressure variation, angular detection accuracy, pulse length, phase errors, plasma processes and variation in meteoroid metallic content are considered. Using computer simulations the observed scatter is reproduced to good accuracy, and then these results are utilized to develop a new procedure that can be used to determine temperatures in the meteor region. These same studies also permit determination of some limited information about the nature of the diffusive expansion process and the variability in the metallic content of meteors. The impact of the quality of phase calibration of interferometric radars on accurate reproduction of atmospheric temperatures is also examined.
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spelling doaj.art-e863763411d5459baed562917805ce462022-12-21T19:27:53ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-11-01223805381410.5194/angeo-22-3805-2004Radar meteor decay rate variability and atmospheric consequencesW. K. Hocking0University of Western Ontario, London, Ontario, CanadaThe reasons for scatter in plots of log(inverse decay times) vs. height for radio meteor echoes are examined, and an explanation for the characteristics is offered. Effects like temperature variability, pressure variation, angular detection accuracy, pulse length, phase errors, plasma processes and variation in meteoroid metallic content are considered. Using computer simulations the observed scatter is reproduced to good accuracy, and then these results are utilized to develop a new procedure that can be used to determine temperatures in the meteor region. These same studies also permit determination of some limited information about the nature of the diffusive expansion process and the variability in the metallic content of meteors. The impact of the quality of phase calibration of interferometric radars on accurate reproduction of atmospheric temperatures is also examined.https://www.ann-geophys.net/22/3805/2004/angeo-22-3805-2004.pdf
spellingShingle W. K. Hocking
Radar meteor decay rate variability and atmospheric consequences
Annales Geophysicae
title Radar meteor decay rate variability and atmospheric consequences
title_full Radar meteor decay rate variability and atmospheric consequences
title_fullStr Radar meteor decay rate variability and atmospheric consequences
title_full_unstemmed Radar meteor decay rate variability and atmospheric consequences
title_short Radar meteor decay rate variability and atmospheric consequences
title_sort radar meteor decay rate variability and atmospheric consequences
url https://www.ann-geophys.net/22/3805/2004/angeo-22-3805-2004.pdf
work_keys_str_mv AT wkhocking radarmeteordecayratevariabilityandatmosphericconsequences