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Optical System Considerations  61

        which is useful for systems where the object and image are not in air.
        If both object and image are in air, we set n   n′   1.0, and recalling
        that f   y 1 /u′, we find

                   h′   u f                                         (4.19)
                         p
                       tan U   f   (for nonparaxial rays)
                             P

        Telescopic magnification
        If we evaluate the invariant at the entrance and exit pupils of a system,
        y p is (by definition) equal to zero, and the invariant becomes

                              Inv   ynu   y′n′u′
                                         p         p
        where y is the pupil semidiameter, and u p is the angular half field of
        view. For an afocal system we can equate the invariant at the entrance
        and exit pupils and then solve for the afocal (or telescopic) angular
        magnification to get
                                       u′     yn
                                         p
                                MP
                                       u
                                        p    y′n′
        which indicates that the telescopic magnification is equal to the ratio
        of entrance pupil diameter to exit pupil diameter (assuming that n   n′).
        This is discussed further in Chap. 13.


        Data of a third ray from two traced rays
        As one might suspect from the preceding, an optical system is actually
        completely defined by the paraxial raytrace data of any two unrelated
        rays, i.e., rays with different axial intersections.
          Paraxial raytrace data may be scaled. In other words the ray
        heights and slopes can be multiplied or divided by a scaling constant;
        the result is a new raytrace. The new ray will still intersect the axis
        at the same point(s) as the old, but the ray heights and slopes will be
        different.
          If we treat raytrace data as just a set of equations, or equalities, it
        is apparent that since one may add or subtract equalities and thereby
        obtain another equality, one can add the scaled data (ray height or
        slope) of two rays and get the data for a third ray. If A and B are scaling
        constants, we can express the data of the third ray as the sum of the
        scaled data of rays 1 and 2.
                                  y   Ay   By                       (4.20)
                                   3     1     2
                                  u 3   Au   Bu                     (4.21)
                                         1     2
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