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Up to this point, the ionosonde signal has been described as though it was a simple pulse. Thinking of it in this way makes understanding the process easier. However, it is difficult to transmit a narrow enough pulse to provide good time resolution, and at the same time provide sufficient energy in the pulse for good sensitivity. This problem is shared with radar systems, and the solutions are similar. In addition, the sounders require to measure the ionosphere throughout the HF spectrum, which is again not so easy to achieve with a pulse.
In the plot, we see that an example frequency of 18.5 MHz, corresponds to a 'chirptime' of 185 seconds (18.5/0.1), meaning that at 18.5 MHz, the chirp will be heard 185s later than the characteristic time for that station.
Peter's design uses the special chirped filter previously described, with properties not attainable with a conventional filter, and so is able to detect the transmissions with 0.66 ms time resolution, and with very narrow bandwidth that provides high sensitivity.
There are two useful advantages of this chirped filter technique:
![]() The graph corresponding to the audio of the chirp in the text |
In the case of conventional chirped ionosondes, the receiver is more
conventional, but follows (tracks) its matching transmitter throughout the
HF spectrum. In this passive sounding project, the receiver tracks many
different transmitters using the chirped filter, but only over the width of
an SSB receiver bandpass - about 2.4 kHz - since the receiver frequency is
fixed. This approach is more than sufficient for sensitive single frequency
measurements. You simply set the receiver frequency to suit the band you
wish to know about. Download and listen to a typical chirp received in a 2.4 kHz bandwidth. |
Copyright Murray Greenman and Peter Martinez, 1999 - 2003 |