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      A Global Geometric Framework for Nonlinear Dimensionality Reduction

      1 , 2 , 3
      Science
      American Association for the Advancement of Science (AAAS)

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          Abstract

          Scientists working with large volumes of high-dimensional data, such as global climate patterns, stellar spectra, or human gene distributions, regularly confront the problem of dimensionality reduction: finding meaningful low-dimensional structures hidden in their high-dimensional observations. The human brain confronts the same problem in everyday perception, extracting from its high-dimensional sensory inputs—30,000 auditory nerve fibers or 10 6 optic nerve fibers—a manageably small number of perceptually relevant features. Here we describe an approach to solving dimensionality reduction problems that uses easily measured local metric information to learn the underlying global geometry of a data set. Unlike classical techniques such as principal component analysis (PCA) and multidimensional scaling (MDS), our approach is capable of discovering the nonlinear degrees of freedom that underlie complex natural observations, such as human handwriting or images of a face under different viewing conditions. In contrast to previous algorithms for nonlinear dimensionality reduction, ours efficiently computes a globally optimal solution, and, for an important class of data manifolds, is guaranteed to converge asymptotically to the true structure.

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          Most cited references24

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          An Information-Maximization Approach to Blind Separation and Blind Deconvolution

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            Nonlinear principal component analysis using autoassociative neural networks

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              Decadal trends in the north atlantic oscillation: regional temperatures and precipitation.

              J Hurrell (1995)
              Greenland ice-core data have revealed large decadal climate variations over the North Atlantic that can be related to a major source of low-frequency variability, the North Atlantic Oscillation. Over the past decade, the Oscillation has remained in one extreme phase during the winters, contributing significantly to the recent wintertime warmth across Europe and to cold conditions in the northwest Atlantic. An evaluation of the atmospheric moisture budget reveals coherent large-scale changes since 1980 that are linked to recent dry conditions over southern Europe and the Mediterranean, whereas northern Europe and parts of Scandinavia have generally experienced wetter than normal conditions.
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                Author and article information

                Journal
                Science
                Science
                American Association for the Advancement of Science (AAAS)
                0036-8075
                1095-9203
                December 22 2000
                December 22 2000
                : 290
                : 5500
                : 2319-2323
                Affiliations
                [1 ]Department of Psychology and
                [2 ]Department of Mathematics, Stanford University, Stanford, CA 94305, USA.
                [3 ]Department of Computer Science, Carnegie Mellon University, Pittsburgh, PA 15217, USA.
                Article
                10.1126/science.290.5500.2319
                11125149
                9e52922d-0eee-4e15-bc4c-d58a270bc513
                © 2000
                History

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