Channel Q function is, for a time-invariant channel, the sum of auto-correlation functions of the channel impulse response functions over multiple receivers. It can be used to characterize the performance (output SNR) of acoustic communications using either passive-phase conjugation or decision feedback equalizer. Channel Q function also determines the channel capacity for a single source and multiple receivers (SIMO). We analyze in this paper that the properties of the channel Q function and show that it possesses a universal and stable properties for underwater acoustic waveguides, irrespective of the channel sound speed profiles, source and receiver range/depths. This property is examined with real data collected in various oceans with significant temporal variations in the propagation conditions and/or source-receiver range. The channel Q function determines the single-source multiple-receivers (SIMO) channel capacity. An example is given for a realistic ocean environment.
[1]
Peter L. Nielsen,et al.
Experimental study of geo-acoustic inversion uncertainty due to ocean sound-speed fluctuations
,
2001
.
[2]
Thomas J. Hayward,et al.
Underwater Acoustic Communication Channel Capacity: A Simulation Study
,
2005
.
[3]
T. C. Yang.
Temporal resolutions of time-reversal and passive-phase conjugation for underwater acoustic communications
,
2003
.
[4]
T.C. Yang,et al.
Differences between passive-phase conjugation and decision-feedback equalizer for underwater acoustic communications
,
2004,
IEEE Journal of Oceanic Engineering.
[5]
Peter L. Nielsen,et al.
Combination of Acoustics with High Resolution Oceanography
,
2002
.
[6]
John G. Proakis,et al.
Digital Communications
,
1983
.