Page 153 - Satellite Communications, Fourth Edition
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Polarization  133

                              local vertical is a complicated function of position, but the following
                              general points can be observed. When the electric field is parallel to the
                              ground (horizontal), t   0, the second term on the right-hand side of the
                              equation for U contributes a  15-dB amount to the XPD, whereas with
                              circular polarization the contribution is only about  0.13 dB. With the
                              electric field vector in the reference plane containing the direction of
                              propagation and the local vertical, t   90°   q (all angles in degrees),
                              and the cos4t term becomes cos4q.



                              5.7 Ice Depolarization
                              As shown in Fig. 4.3 an ice layer is present at the top of a rain region,
                              and as noted in Table 4.1, the ice crystals can result in depolarization.
                              The experimental evidence suggests that the chief mechanism pro-
                              ducing depolarization in ice is differential phase shift, with little dif-
                              ferential attenuation present. This is so because ice is a good dielectric,
                              unlike water, which has considerable losses. Ice crystals tend to be
                              needle-shaped or platelike and, if randomly oriented, have little effect,
                              but depolarization occurs when they become aligned. Sudden increases
                              in XPD that coincide with lightning flashes are thought to be a result
                              of the lightning producing alignment.  An  International Radio
                              Consultative Committee (CCIR) recommendation for taking ice depo-
                              larization into account is to add a fixed decibel value to the XPD value
                              calculated for rain. Values of 2 dB are suggested for North America and
                              4 to 5 dB for maritime regions, and it is further suggested that the
                              effects of ice can be ignored for time percentages less than 0.1 percent
                              (Ippolito, 1986).



                              5.8 Problems and Exercises
                              5.1.  Explain what is meant by a plane TEM wave.

                              5.2. Two electric fields, in time phase and each of unity amplitude, act at right
                              angles to one another in space. On a set of x-y axes draw the path traced by the
                              tip of the resultant electric field vector. Given that the total power developed
                              across a 50 Ω load is 5 W, find the peak voltage corresponding to the unity
                              amplitude.
                              5.3.  Two electric fields with an amplitude ratio of 3:1 and in time phase, act
                              at right angles to one another in space. On a set of x-y axes draw the path
                              traced by the tip of the resultant. Given that the total power developed across
                              a 50 Ω load is 10 W, find the peak voltage corresponding to the unity
                              amplitude.
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