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222                                     UNSUPERVISED LEARNING

            2. Gradient descent
                                (t)
              . For each object y , calculate the gradient according to (7.6).
                                i
                                            (t)
                                (t)
              . Update: y (tþ1)  ¼ y    qE S =qy , where   is a learning rate.
                         i
                                            i
                                i
              . As long as E S significantly decreases, set t ¼ t þ 1 and go to step 2.
            Figures 7.3(a) to (c) show examples of two-dimensional MDS mapping.
            The data set, given in Table 7.1, consists of the geodesic distances of 13
            world cities. These distances can only be fully brought in accordance
            with the true three-dimensional geographical positions of the cities if the
            spherical surface of the earth is accounted for. Nevertheless, MDS
            has found two-dimensional mappings that resemble the usual Mercator
            projection of the earth surface on the tangent plane at the North Pole.
              Since distances are invariant to translation, rotation and mirroring,
            MDS can result in arbitrarily shifted, rotated and mirrored mappings.


                            q =– 2                          q =0
                                                                Melbourne
             8000              Honolulu       8000    Honolulu
                           Los Angeles
             4000                     Tokyo   4000        Los Angeles
                             Melbourne                               Tokyo
                                       Beijing
                     New York                            New York     Beijing
                0                                0 Santiago
                    Santiago  London  Bangkok                       Bangkok
                                 Moscow             Rio    London Moscow
             –4000    Rio                    –4000
                                  Cairo                         Cairo
             –8000                           –8000
                            Capetown                      Capetown
                  –8000 –4000  0  4000 8000       –8000 –4000  0  4000 8000


                            q =2                           D =3; q =0
                                   Melbourne
             8000       Honolulu
                                                         Los Angeles
                                                  New York        Honolulu
                           Los Angeles
             4000 Santiago                                            Tokyo
                                                           London
                                       Tokyo               London     Beijing
                                                           London
                                                              Moscow
                                                              Moscow
                                                              Moscow
                                       Beijing
                0        New York              Santiago
                                                             Cairo
                                                             Cairo
                     Rio             Bangkok     Rio         Cairo   Bangkok
                           London
             –4000               Moscow                             Melbourne
                                Cairo
                                                            Capetown
             –8000
                              Capetown
                  –8000 –4000  0  4000  8000
            Figure 7.3  MDS applied to a matrix of geodesic distances of world cities
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