chapter 12, Laser Satellite Communication Systems

In Part II Applications from: Laser Beam Propagation through Random Media
Author(s): Larry C. Andrews, Ronald L. Phillips

Chapter Contents

  • 12.1 Introduction
  • 12.2 Atmospheric Channels
  • 12.3 Background
  • 12.4 Second-Order Statistics
  • 12.5 Irradiance Statistics: Downlink Channel
  • 12.6 Irradiance Statistics: Uplink Channel
  • 12.7 Fade Statistics: Downlink Channels
  • 12.8 Fade Statistics: Uplink Channels
  • 12.9 Summary and Discussion
  • 12.10 Worked Examples
  • Problems
  • References

Excerpt

Overview: In this chapter we consider statistical quantities introduced in Chaps. 6–9 and adapt them to vertical and slant path propagation links. Most of the analysis presented here is for a slant path connecting a satellite in geostationary orbit and a ground or airborne platform. The uplink and downlink paths for such links are vastly different because the atmospheric turbulence layer is only near the transmitter on an uplink path and only near the receiver on a downlink path. This difference in path for the two cases leads to important differences in the derived expressions for beam spreading, scintillation index, spatial coherence radius of the wave, and the effect these parameters have on the probability of fade. In particular, we examine the effect that beam wander has on the scintillation index of an uplink path to space and its implications on fading statistics.

The greatest difference in modeling uplink/downlink paths (or general slant paths) compared with horizontal propagation paths is that in the former we need to consider changes in the refractive index structure parameter Cn2 along the path. Generally, changes in Cn2 along the path can be inferred from a profile model of Cn2 as a function of altitude. In our work here we rely on the Hufnagle-Valley Cn2 profile model, but this is not essential for the general analysis. We choose this model because it offers a little more generality than other Cn2 profile models through the use of two independent parameters identifying ground-level Cn2 values and upper atmospheric wind speeds.

Weak fluctuation theory based on the Rytov approximation is sufficient for most of the calculations required in the analysis of an uplink or downlink path provided the zenith angle is sufficiently small (less than 60 deg in most cases but may be restricted to zenith angles less than 45 deg in cases where ground-level Cn2 is large). However, it may be necessary to use strong fluctuation models for large-diameter beams in the presence of beam wander effects, and/or large zenith angles such as those that occur in near-horizon propagation paths.



©2005 Society of Photo-Optical Instrumentation Engineers
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Print ISBN:

9780819459480

Print ISBN:

0819459488

eISBN:

9780819478320

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