Determination of meteoroid physical properties from tristatic radar observations

In this work we give a review of the meteor head echo observations carried out with the tristatic 930 MHz EISCAT UHF radar system during four 24 h runs between 2002 and 2005 and compare these with earlier observations. A total number of 410 tristatic meteors were observed. We describe a method to de...

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Published in:Annales Geophysicae
Main Authors: Kero, J., Szasz, C., Pellinen-Wannberg, A., Wannberg, G., Westman, A., Meisel, D. D.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-26-2217-2008
https://angeo.copernicus.org/articles/26/2217/2008/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo36480 2023-05-15T16:04:45+02:00 Determination of meteoroid physical properties from tristatic radar observations Kero, J. Szasz, C. Pellinen-Wannberg, A. Wannberg, G. Westman, A. Meisel, D. D. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-26-2217-2008 https://angeo.copernicus.org/articles/26/2217/2008/ eng eng doi:10.5194/angeo-26-2217-2008 https://angeo.copernicus.org/articles/26/2217/2008/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-26-2217-2008 2020-07-20T16:26:51Z In this work we give a review of the meteor head echo observations carried out with the tristatic 930 MHz EISCAT UHF radar system during four 24 h runs between 2002 and 2005 and compare these with earlier observations. A total number of 410 tristatic meteors were observed. We describe a method to determine the position of a compact radar target in the common volume monitored by the three receivers and demonstrate its applicability for meteor studies. The inferred positions of the meteor targets have been utilized to estimate their velocities, decelerations and directions of arrival as well as their radar cross sections with unprecedented accuracy. The velocity distribution of the meteoroids is bimodal with peaks at 35–40 km/s and 55–60 km/s, and ranges from 19–70 km/s. The estimated masses are between 10 −9 –10 −5.5 kg. There are very few detections below 30 km/s. The observations are clearly biased to high-velocity meteoroids, but not so biased against slow meteoroids as has been presumed from previous tristatic measurements. Finally, we discuss how the radial deceleration observed with a monostatic radar depends on the meteoroid velocity and the angle between the trajectory and the beam. The finite beamwidth leads to underestimated meteoroid masses if radial velocity and deceleration of meteoroids approaching the radar are used as estimates of the true quantities in a momentum equation of motion. Text EISCAT Copernicus Publications: E-Journals Annales Geophysicae 26 8 2217 2228
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description In this work we give a review of the meteor head echo observations carried out with the tristatic 930 MHz EISCAT UHF radar system during four 24 h runs between 2002 and 2005 and compare these with earlier observations. A total number of 410 tristatic meteors were observed. We describe a method to determine the position of a compact radar target in the common volume monitored by the three receivers and demonstrate its applicability for meteor studies. The inferred positions of the meteor targets have been utilized to estimate their velocities, decelerations and directions of arrival as well as their radar cross sections with unprecedented accuracy. The velocity distribution of the meteoroids is bimodal with peaks at 35–40 km/s and 55–60 km/s, and ranges from 19–70 km/s. The estimated masses are between 10 −9 –10 −5.5 kg. There are very few detections below 30 km/s. The observations are clearly biased to high-velocity meteoroids, but not so biased against slow meteoroids as has been presumed from previous tristatic measurements. Finally, we discuss how the radial deceleration observed with a monostatic radar depends on the meteoroid velocity and the angle between the trajectory and the beam. The finite beamwidth leads to underestimated meteoroid masses if radial velocity and deceleration of meteoroids approaching the radar are used as estimates of the true quantities in a momentum equation of motion.
format Text
author Kero, J.
Szasz, C.
Pellinen-Wannberg, A.
Wannberg, G.
Westman, A.
Meisel, D. D.
spellingShingle Kero, J.
Szasz, C.
Pellinen-Wannberg, A.
Wannberg, G.
Westman, A.
Meisel, D. D.
Determination of meteoroid physical properties from tristatic radar observations
author_facet Kero, J.
Szasz, C.
Pellinen-Wannberg, A.
Wannberg, G.
Westman, A.
Meisel, D. D.
author_sort Kero, J.
title Determination of meteoroid physical properties from tristatic radar observations
title_short Determination of meteoroid physical properties from tristatic radar observations
title_full Determination of meteoroid physical properties from tristatic radar observations
title_fullStr Determination of meteoroid physical properties from tristatic radar observations
title_full_unstemmed Determination of meteoroid physical properties from tristatic radar observations
title_sort determination of meteoroid physical properties from tristatic radar observations
publishDate 2018
url https://doi.org/10.5194/angeo-26-2217-2008
https://angeo.copernicus.org/articles/26/2217/2008/
genre EISCAT
genre_facet EISCAT
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-26-2217-2008
https://angeo.copernicus.org/articles/26/2217/2008/
op_doi https://doi.org/10.5194/angeo-26-2217-2008
container_title Annales Geophysicae
container_volume 26
container_issue 8
container_start_page 2217
op_container_end_page 2228
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