v2007.09.13 - Convex Optimization

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

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368 CHAPTER 5. EUCLIDEAN DISTANCE MATRIXD(X) = D(X[0 √ 2V N ]) = D(Q p [0 √ ΛQ T ]) = D([0 √ ΛQ T ]) (937)This suggests a way to find EDM D given −V T N DV N ; (confer (818))[0D =δ ( −VN TDV )N] [1 T + 1 0 δ ( −VN TDV ) ] TN[ 0 0T− 20 −VN TDV N(725)]5.12.2 0 geometric center. VAlternatively, we may perform reconstruction using instead the auxiliarymatrix V (B.4.1), corresponding to the polyhedronP − α c (938)whose geometric center has been translated to the origin. Redimensioningdiagonalization factors Q, Λ∈R N×N and unknown Q p ∈ R n×N , (841)−V DV = 2V X T XV ∆ = Q √ ΛQ T pQ p√ΛQT ∆ = QΛQ T (939)where the geometrically centered generating list constitutes (confer (935))XV = 1 √2Q p√ΛQ T ∈ R n×N= [x 1 − 1 N X1 x 2 − 1 N X1 x 3 − 1 N X1 · · · x N − 1 N X1 ] (940)where α c = 1 N X1. (5.5.1.0.1) The simplest choice for Q p is [I 0 ]∈ R r×N .Now EDM D can be uniquely made from the list found, by calculating:(705)D(X) = D(XV ) = D( 1 √2Q p√ΛQ T ) = D( √ ΛQ T ) 1 2(941)This EDM is, of course, identical to (937). Similarly to (725), from −V DVwe can find EDM D ; (confer (805))D = δ(−V DV 1 2 )1T + 1δ(−V DV 1 2 )T − 2(−V DV 1 2 ) (731)

5.12. LIST RECONSTRUCTION 369(a)(c)(b)(d)(f)(e)Figure 90: Map of United States of America showing some state boundariesand the Great Lakes. All plots made using 5020 connected points. Anydifference in scale in (a) through (d) is an artifact of plotting routine.(a) shows original map made from decimated (latitude, longitude) data.(b) Original map data rotated (freehand) to highlight curvature of Earth.(c) Map isometrically reconstructed from the EDM.(d) Same reconstructed map illustrating curvature.(e)(f) Two views of one isotonic reconstruction; problem (950) with no sortconstraint Πd (and no hidden line removal).

5.12. LIST RECONSTRUCTION 369(a)(c)(b)(d)(f)(e)Figure 90: Map of United States of America showing some state boundariesand the Great Lakes. All plots made using 5020 connected points. Anydifference in scale in (a) through (d) is an artifact of plotting routine.(a) shows original map made from decimated (latitude, longitude) data.(b) Original map data rotated (freehand) to highlight curvature of Earth.(c) Map isometrically reconstructed from the EDM.(d) Same reconstructed map illustrating curvature.(e)(f) Two views of one isotonic reconstruction; problem (950) with no sortconstraint Πd (and no hidden line removal).

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