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Radiometry, Wave Optics, and Spatial Coherence     219


                 For a planar source of area Aand in the plane z = constant, the total
               radiant power is defined by the integral over the area of the source

                                  (z) =    M(x, y, z) dx dy          (7.3)
                                        A
                 On the other hand, the radiation from the source is received on a
               surface. It is described by the term radiant incidence or irradiance E with
                           −2
               units of W cm . It too is a function of position  r. The spectral irradiance
                                     −2
                                         −1
                ˆ E( r,  ) has units of W cm Hz .
                 Let us reconsider the radiant exitance M. It is a function of position
                                                 ˆ
                                       r = ˆ ix + ˆ jy + kz          (7.4)
                 From every point (x, y) on the source, it may channel different
               amounts of radiation energy in different directions ˆ n with compo-
               nents
                                       ˆ
                           ˆ n = ˆ ip + ˆ jq + km
                                                                     (7.5)
                                                        ˆ
                             = ˆ i(sin   cos 	) + ˆ j(sin   sin 	) + k cos
               where   and 	 are the polar angles,   is measured from the z axis, and
               the azimuthal angle 	 is measured from the x axis in the xy plane.
               The differential element of solid angle d	 with units of steradians (sr)
               about the direction ˆ n is

                                       dp dq
                                 d	 =       = sin   d  d	            (7.6)
                                        m
               This equality is established by using the Jacobian of the change of
               variables from ( p, q)to ( , 	).
                 To account for the variation of the source properly as a function
               of position and direction, a term called radiance L( r, ˆ n) is used, with
                              −1
                           −2
               units of W cm sr . An observer looking at the source in the direction
               of ˆ n sees the projected area dA proj = dA cos  as shown in Fig. 7.1.


                                  dA proj  = dA cosq
                                                        ˆ n

                              dA             q     dW




               FIGURE 7.1 Projected area.
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