Volume 2, Weak Scattering
By Albert D. Wheelon
Publisher: Cambridge University Press
Print Publication Year: 2003
Online Publication Date:December 2009
Chapter DOI: http://dx.doi.org/10.1017/CBO9780511534812.007
The wavelength scaling of amplitude variance discussed in Section 3.2.4 was found to give good agreement between theory and experiment. We can take this comparison one step further and compare the detailed variations of amplitude at two wavelengths. The amplitude histories for radio-astronomical signals at 81.5 and 118.5 MHz received from a radio source in Cassiopeia  are reproduced in Figure 6.1. Investigations of this correlated signal behavior were originally driven by practical considerations. Radio astronomers working with very faint signals wanted to know how wide a frequency band they could use to improve the signal-to-noise ratio. Engineers designing terrestrial and satellite communication relay links wondered whether turbulence scattering would limit the information bandwidth that could be transmitted through the atmosphere.
Both questions are related to the medium bandwidth which measures the frequency separation over which received signals behave in the same way. Severe medium-bandwidth limitations had been observed on tropospheric and ionospheric scatter-propagation circuits. That experience raised the possibility that only a narrow slice of frequency spectrum would be coherent and thus useful for line-of-sight transmissions. Experimental data showed instead that a very large bandwidth should be available . For weak scattering the signal strength is correlated over a wide range of frequencies because the strong coherent field provides a powerful stabilizing reference – as it cannot for scatter propagation.
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