A method for restoration of radio channel transfer function by chirp sounding of the ionosphere

Abstract

1] Analysis of both in-phase and quadrature components of received frequency-modulated continuous wave (FMCW) signal at the output of intermediate frequency (IF) band-pass filter of the chirp ionosonde demonstrates a new possibility of recovering the transfer function of the HF radio channel within the band of operating frequencies and the interval of time delays that are defined by the IF filter characteristics. The transfer function is determined by the parameters of all parts comprising the radio channel: transmitter, receiving-transmitting antenna-feeder devices, Earth surface, ionosphere, as well as the receiver circuitry participating in the signal processing. However, characteristics of all parts except the ionosphere can be considered stationary and well-known or controlled. It is the ionosphere that displays significant temporal variability. A new technique is proposed for recovering the transfer function of the ionospheric radio channel, together with its implementation as a signal preprocessing circuit containing a correcting digital filter that adapts to the current amplitude frequency and phase frequency characteristics of the channel. INDEX TERMS: 2441 Ionosphere: Ionospheric storms; 2407 Ionosphere: Auroral ionosphere; 2447 Ionosphere: Modeling and forecasting; KEYWORDS: FMCW sounder, chirp sounding technique, ionospheric radio channel, transfer function, digital signal processing. Citation: Davydenko, M. A., N. V. Ilyin, and V. V. Khakhinov (2008), A method for restoration of radio channel transfer function by chirp sounding of the ionosphere, Int.

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“…In our case, there is no limitation on the type of signal characteristics as long as it has at least a segment of a continuous IF track in the time‐frequency plane which is not corrupted by other sources. Nevertheless, we consider constant amplitude frequency modulated (FM) signals like s k ( t ) = α ( t ) for k = 1,…, n which are used in ionosphere sounding [ Davydenko et al , 2008]. The instantaneous frequency for the source signal is to be found automatically by using the STFT distribution of the signals.…”

“…Nevertheless, we consider constant amplitude frequency modulated (FM) signals like s k (t) = a k e j8 k (t) for k = 1,. . ., n which are used in ionosphere sounding [Davydenko et al, 2008]. The instantaneous frequency for the source signal is to be found automatically by using the STFT distribution of the signals.…”