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272   Chapter Eight


               simplified model for the square of the refractive index
                                  $  2
                                    n                  x ≥ x 0
                            2        0
                           n (x) =                                 (8.103)
                                                  2
                                           2
                                     2
                                    n [1 −   (x − x 0 ) ]
                                     0                 x < x 0
               where x 0 is the height at which the refractive index becomes constant
               and   determines the speed of the variation of the refractive index
               near x = 0. Consider a point source located at (x s , 0), where x s >
                x 0 , emitting light uniformly in all directions. Let us choose the ray
               parameter   as the angle (with respect to the z axis) at which each ray
               leaves the source. Since the refractive index is independent of z, H is
               invariant under propagation, according to Eq. (8.19c). From geometry,
               its value is found to be
                                      H( ) = n 0 cos               (8.104)
               The solutions to Eqs. (8.19a), (8.19b), and (8.20) take different forms in
               three regions:

                  1. If the ray has not entered the inhomogeneous region x < x 0 ,
                    then it is a straight line defined by

                                      X(z,  ) = x s + z tan        (8.105a)
                                      P(z,  ) = n 0 sin           (8.105b)
                                      L(z,  ) = n 0 z sec          (8.105c)

                  2. If the ray is inside the inhomogeneous region, then
                                   sin
                       X(z,  ) = x 0 +  sin{ [z − Z 1 ( )] sec  }  (8.106a)

                       P(z,  ) = n 0 sin   cos{ [z − Z 1 ( )] sec  }  (8.106b)

                                                  sin
                       L(z,  ) = n 0 sec    Z 1 ( ) + 1 +  [z − Z 1 ( )]
                                                    2
                                 n 0
                               +   sin   sin{2 [z − Z 1 ( )] sec  }  (8.106c)
                                 4
                    where Z 1 ( ) = (x s − x 0 ) cot   is the value of z at which the ray
                    enters the inhomogeneous region.
                  3. If the ray has entered and exited the inhomogeneous region,
                    then
                      X(z,  ) = x 0 − [z − Z 2 ( )] tan            (8.107a)

                      P(z,  ) =−n 0 sin                           (8.107b)

                                                       n 0    sin
                      L(z,  ) = n 0 [z + Z 1 ( ) − Z 2 ( )] sec   +  1 +
                                                                2
                                                                   (8.107c)
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