v2007.09.13 - Convex Optimization

v2007.09.13 - Convex Optimization v2007.09.13 - Convex Optimization

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372 CHAPTER 5. EUCLIDEAN DISTANCE MATRIXλ(−V T N OV N) j90080070060050040030020010001 2 3 4 5 6 7 8 9 10jFigure 91: Largest ten eigenvalues of −VN TOV N for map of USA, sorted bynonincreasing value. In the code (F.3.2), we normalize O by (N(N −1)/2) 2 .Any process of reconstruction that leaves comparative distanceinformation intact is called ordinal multidimensional scaling or isotonicreconstruction. Beyond rotation, reflection, and translation error, (5.5)list reconstruction by isotonic reconstruction is subject to error in absolutescale (dilation) and distance ratio. Yet Borg & Groenen argue: [39,2.2]reconstruction from complete comparative distance information for a largenumber of points is as highly constrained as reconstruction from an EDM;the larger the number, the better.5.13.2.1 Isotonic map of the USATo test Borg & Groenen’s conjecture, suppose we make a complete sort-indexmatrix O ∈ S N h ∩ R N×N+ for the map of the USA and then substitute O in placeof EDM D in the reconstruction process of5.12. Whereas EDM D returnedonly three significant eigenvalues (943), the sort-index matrix O is generallynot an EDM (certainly not an EDM with corresponding affine dimension 3)so returns many more. The eigenvalues, calculated with absolute numericalerror approximately 5E-7, are plotted in Figure 91:λ(−V T N OV N ) = [880.1 463.9 186.1 46.20 17.12 9.625 8.257 1.701 0.7128 0.6460 · · · ] T(948)

5.13. RECONSTRUCTION EXAMPLES 373The extra eigenvalues indicate that affine dimension corresponding to anEDM near O is likely to exceed 3. To realize the map, we must simultaneouslyreduce that dimensionality and find an EDM D closest to O in some sense(a problem explored more in7) while maintaining the known comparativedistance relationship; e.g., given permutation matrix Π expressing theknown sorting action on the entries d of unknown D ∈ S N h , (63)d ∆ = 1 √2dvec D =⎡⎢⎣⎤d 12d 13d 23d 14d 24d 34⎥⎦.d N−1,N∈ R N(N−1)/2 (949)we can make the sort-index matrix O input to the optimization problemminimize ‖−VN T(D − O)V N ‖ FDsubject to rankVN TDV N ≤ 3(950)Πd ∈ K M+D ∈ EDM Nthat finds the EDM D (corresponding to affine dimension not exceeding 3 inisomorphic dvec EDM N ∩ Π T K M+ ) closest to O in the sense of Schoenberg(724).Analytical solution to this problem, ignoring the sort constraintΠd ∈ K M+ , is known [262]: we get the convex optimization [sic] (7.1)minimize ‖−VN T(D − O)V N ‖ FDsubject to rankVN TDV N ≤ 3(951)D ∈ EDM NOnly the three largest nonnegative eigenvalues in (948) need be retainedto make list (935); the rest are discarded. The reconstruction fromEDM D found in this manner is plotted in Figure 90(e)(f) from which itbecomes obvious that inclusion of the sort constraint is necessary for isotonicreconstruction.

372 CHAPTER 5. EUCLIDEAN DISTANCE MATRIXλ(−V T N OV N) j90080070060050040030020010001 2 3 4 5 6 7 8 9 10jFigure 91: Largest ten eigenvalues of −VN TOV N for map of USA, sorted bynonincreasing value. In the code (F.3.2), we normalize O by (N(N −1)/2) 2 .Any process of reconstruction that leaves comparative distanceinformation intact is called ordinal multidimensional scaling or isotonicreconstruction. Beyond rotation, reflection, and translation error, (5.5)list reconstruction by isotonic reconstruction is subject to error in absolutescale (dilation) and distance ratio. Yet Borg & Groenen argue: [39,2.2]reconstruction from complete comparative distance information for a largenumber of points is as highly constrained as reconstruction from an EDM;the larger the number, the better.5.13.2.1 Isotonic map of the USATo test Borg & Groenen’s conjecture, suppose we make a complete sort-indexmatrix O ∈ S N h ∩ R N×N+ for the map of the USA and then substitute O in placeof EDM D in the reconstruction process of5.12. Whereas EDM D returnedonly three significant eigenvalues (943), the sort-index matrix O is generallynot an EDM (certainly not an EDM with corresponding affine dimension 3)so returns many more. The eigenvalues, calculated with absolute numericalerror approximately 5E-7, are plotted in Figure 91:λ(−V T N OV N ) = [880.1 463.9 186.1 46.20 17.12 9.625 8.257 1.701 0.7128 0.6460 · · · ] T(948)

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