Satellite Communications, Fourth Edition

Chapter 4: Radio Wave Propagation

4.1 Introduction

A signal traveling between an earth station and a satellite must pass through the earth s atmosphere, including the ionosphere, as shown in Fig. 4.1, and this can introduce certain impairments, which are summarized in Table 4.1. Some of the more important of these impairments will be described in this chapter.


Figure 4.1: Layers in the earth s atmosphere.
Table 4.1: Propagation Concerns for Satellite Communications Systems
Propagation impairment Physical cause Prime importance

Attenuation and sky noise increases

Atmospheric gases, cloud, rain

Frequencies above about 10 GHz

Signal depolarization

Rain, ice crystals

Dual-polarization systems at C and Ku bands (depends on system configuration)

Refraction, atmospheric multipath

Atmospheric gases

Communication and tracking at low elevation angles

Signal scintillations

Tropospheric and ionospheric refractivity fluctuations

Tropospheric at frequencies above 10 GHz and low-elevation angles; ionospheric at frequencies below 10 GHz

Reflection multipath, blockage

Earth s surface, objects on surface

Mobile satellite services

Propagation delays, variations

Troposphere, ionosphere

Precise timing and location systems; time division multiple access (TDMA) systems

Intersystem interference

Ducting, scatter, diffraction

Mainly C band at present; rain scatter may be significant at higher frequencies

SOURCE: Brussard and Rogers, 1990.

4.2 Atmospheric Losses

Losses occur in the earth s atmosphere as a result of energy absorption by the atmospheric gases. These losses are treated quite separately from those which result from adverse weather conditions, which of course are also atmospheric losses. To distinguish between these, the weather-related losses are referred to as atmospheric attenuation

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