Meteor Wind Radar
In October
2000 a SKiYMET All-Sky Imager VHF Meteor Wind Radar (MWR) was deployed at
BLO for comparative measurements of MLT winds and temperature in collaboration
with Prof. Wayne Hocking, University of Western Ontario (UWO), Canada. The radar
system is autonomous and operates continuously. Collaborative measurements were
completed in April, 2001.
The MWR used pulsed radio waves transmitted from a broad-beamed antenna to
detect meteor trails in the MLT region (~80-100 km). By comparing the reflected
signals, the position of each meteor trail can be computed to determine wind
speeds as a function of height (e.g. Hocking, 1997). The flux of meteor echoes
peaks during the night and is generally in excess of 300/hr decreasing near
07 LT.
As discussed by Hocking (2000), the SKiYMET system is unique in that it utilizes
interferometry and a high pulse repetition frequency for these measurements.
The MWR was configured for operation at 35.65 MHz (a Yellowknife operational
requirement) and sometimes suffers from co-channel interference during the day
(07-17 LT), thereby reducing the expected meteor detection rate. The MWR winds
are derived at 1-hour intervals at heights centered on 85, 88, 91 and 94 km.
This data was utilized, among other science objectives, to validate the winds
derived with the BLO dynasonde (operating in IDI mode). In addition to wind
measurements between 85-95 km, the MWR data on the meteor decay times can be
used to estimate mesospheric temperatures (Hocking, et al., 1997; Hocking, 1999).
Work is currently in progress to compare the temperatures derived from the MWR
data with those determined by the Mesospheric Temperature Mapper.
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