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N.L.O. Meteor Detection Live View

Meteor Detection


When a meteor strikes Earth’s atmosphere it decelerates rapidly. The friction created by the air causes the meteor to burn up at extremely high temperatures creating the white “shooting star” that we are all familiar with. This process also ionises the air along the trail making it possible to reflect radio waves.


Utilising a high powered VHF radar signal sent into the sky, we are able to detect reflected waves from these ionisation trails. Because the meteor is moving, the reflected signal is shifted in frequency from the original, by an amount according to it’s speed. This shift is also heard as an audible ping by the station operator.


Our system translates the reflected wave into three main parameters - Amplitude (strength), Frequency shift (Doppler shift) and decay time. This allows us to determine the relative size of the meteor strike (vertical scale) and the relative approximate speed and deceleration (amount of shift and width of the trace).


You can see the output from our system above in real time (approximately 1 minute delay on the Internet). During a meteor shower this trace will be full of strike traces, but it is also surprising how many meteors are striking Earth’s atmosphere all of the time.

Typical Meteor Strike


Here you can see what a typical meteor strike looks like. The trace starts high in frequency and rapidly drops to the radar carrier frequency as the meteor decelerates in the atmosphere, increasing in strength (ionisation) as it burns up. This creates this typical triangular shape you can see here. The width, height and shape tell us a lot about the meteor strike. The blue is the baseline atmospheric noise.

Meteor Showers in 2013


Quadrantids - January 3rd

Lyrids - April 21/22

Eta Aquarids - May 5/6th

Perseids - August 12th

Orionids - October 21st

Leonids - November 17th

Geminids - December 13th

Click here for NLO - S.P.A.M. network multiscreen