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The Canadian Meteor Orbit Radar Meteor Stream Catalogue
Earth, Moon, and Planets, 2007The Canadian Meteor Orbit Radar is a multi-frequency backscatter radar which has been in routine operation since 1999, with an orbit measurement capability since 2002. In total, CMOR has measured over 2 million orbits of meteoroids with masses greater than 10 μg, while recording more than 18 million meteor echoes in total.
Peter Brown +3 more
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The observations of Kunming meteor radar and height distribution of meteor
Proceedings of the 9th International Symposium on Antennas, Propagation and EM Theory, 2010Based on the meteor radar, one can study the radiant distribution and the time variant of meteors, investigate space debris and predict the passage time of meteor showers, and so on. By observation of the Kunming meteor radar, the observation data of meteor decay time and the ambipolar diffusion coefficient are consistent with the theories.
null Yun Liu +5 more
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The French meteor radar facility
Journal of Atmospheric and Terrestrial Physics, 1978Abstract A brief history of the meteor radars developed by the National Center for Telecommunication Studies is followed by a description of the equipment and data analysis techniques. Details are given of the simultaneously measured radio meteor winds over Garchy, France (47°N, 3°E) and Kiruna, Sweden (68°N, 20°E) during August 1974, and over Garchy
M. Glass +3 more
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Time–Frequency Radar Processing for Meteor Detection
IEEE Transactions on Geoscience and Remote Sensing, 2004In this paper, we present signal processing techniques to detect meteor returns from Arecibo Observatory 430-MHz UHF radar data. We exploit the characteristics of the transmit waveform in the frequency domain as well as in the time domain. Two detection methods are investigated.
Chun-Hsien Wen +2 more
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Radar Detection of Meteor Trails
Nature, 1946IN the course of ionospheric observations made during the International Polar Year 1932–33, a transient type of radio echo was observed from levels in the upper atmosphere about 100 km. above the ground. Such echoes were found to last only a second or two and were noted to be equally frequent both by day and by night.
EDWARD APPLETON, R. NAISMITH
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SDR-based radar system for meteor detection
2009 16th International Conference on Digital Signal Processing, 2009The idea of monitoring atmospheric events using radio waves has been implemented in the past. The concept has also been employed to detect meteors, that is, ionized trails created by meteors. The approach exploits the property of ionized trails to reflect radio waves and the use of bistatic radar and forward scattering. In this paper we present a setup
Subodh Chiwate +8 more
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The Poker Flat, Alaska, MST radar as a meteor radar
Radio Science, 1983Meteor echoes received on the mesosphere‐stratosphere‐troposphere radar at Poker Flat, Alaska, have been tested for their usefulness in studying the large‐scale dynamics of the upper mesosphere and lower ionosphere. A selection scheme has been developed to extract meteor echoes from the normally observed turbulence scatter echoes in a composite data ...
S. K. Avery, A. C. Riddle, B. B. Balsley
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Antarctic meteor observations using the Davis MST and meteor radars
Advances in Space Research, 2008Abstract This paper presents the meteor observations obtained using two radars installed at Davis (68.6°S, 78.0°E), Antarctica. The Davis MST radar was installed primarily for observation of polar mesosphere summer echoes, with additional transmit and receive antennas installed to allow all-sky interferometric meteor radar observations.
Holdsworth, D. +3 more
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Radar observations of meteor deceleration
Journal of Geophysical Research, 1966By using a narrow-beam high-power radar operating at 68 cm it has been possible to detect meteors traveling radially toward the radar. In these observations the antenna is directed at the radiant point of an intense meteor shower, and the receiver is tuned to the expected Doppler-shifted signal.
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Meteor wind observations with the MU radar
Radio Science, 1991We conducted meteor wind observations with the middle and upper atmosphere (MU) radar at Shigaraki, Japan (35°N, 136°E), utilizing an interferometer to determine the arrival angle of a meteor echo. We found that meteor echoes are widely distributed in zenith angles as large as 50° and that the narrow main lobe of a transmitting antenna cannot ...
T. Nakamura +6 more
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