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Properties of EMD Basis

Properties of EMD Basis. The Adaptive Basis based on and derived from the data by the empirical method satisfy nearly all the traditional requirements for basis empirically and a posteriori : Complete Convergent Orthogonal Unique.

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Properties of EMD Basis

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  1. Properties of EMD Basis The Adaptive Basis based on and derived from the data by the empirical method satisfy nearly all the traditional requirements for basis empirically and a posteriori: Complete Convergent Orthogonal Unique

  2. The combination of Hilbert Spectral Analysis and Empirical Mode Decomposition has been designated by NASA as HHT (HHT vs. FFT)

  3. Comparison between FFT and HHT

  4. Comparisons: Fourier, Hilbert & Wavelet

  5. Surrogate Signal:Non-uniqueness signal vs. Spectrum I. Hello

  6. The original data : Hello

  7. The IMF of original data : Hello

  8. The surrogate data : Hello

  9. The IMF of Surrogate data : Hello

  10. The Hilbert spectrum of original data : Hello

  11. The Hilbert spectrum of Surrogate data : Hello

  12. To quantify nonlinearity we also need instantaneous frequency. Additionally

  13. How to define Nonlinearity? How to quantify it through data alone (model independent)?

  14. The term, ‘Nonlinearity,’ has been loosely used, most of the time, simply as a fig leaf to cover our ignorance. Can we be more precise?

  15. How is nonlinearity defined? Based on Linear Algebra: nonlinearity is defined based on input vs. output. But in reality, such an approach is not practical: natural system are not clearly defined; inputs and out puts are hard to ascertain and quantify. Furthermore, without the governing equations, the order of nonlinearity is not known. In the autonomous systems the results could depend on initial conditions rather than the magnitude of the ‘inputs.’ The small parameter criteria could be misleading: sometimes, the smaller the parameter, the more nonlinear.

  16. Linear Systems Linear systems satisfy the properties of superpositionand scaling. Given two valid inputs to a system H, as well as their respective outputs then a linear system, H, must satisfy for any scalar values α and β.

  17. How is nonlinearity defined? Based on Linear Algebra: nonlinearity is defined based on input vs. output. But in reality, such an approach is not practical: natural system are not clearly defined; inputs and out puts are hard to ascertain and quantify. Furthermore, without the governing equations, the order of nonlinearity is not known. In the autonomous systems the results could depend on initial conditions rather than the magnitude of the ‘inputs.’ The small parameter criteria could be misleading: sometimes, the smaller the parameter, the more nonlinear.

  18. How should nonlinearity be defined? The alternative is to define nonlinearity based on data characteristics: Intra-wave frequency modulation. Intra-wave frequency modulation is known as the harmonic distortion of the wave forms. But it could be better measured through the deviation of the instantaneous frequency from the mean frequency (based on the zero crossing period).

  19. Characteristics of Data from Nonlinear Processes

  20. Duffing Pendulum x

  21. Duffing Equation : Data

  22. Hilbert’s View on Nonlinear DataIntra-wave Frequency Modulation

  23. A simple mathematical model

  24. Duffing Type WaveData:x = cos(wt+0.3 sin2wt)

  25. Duffing Type WavePerturbation Expansion

  26. Duffing Type WaveWavelet Spectrum

  27. Duffing Type WaveHilbert Spectrum

  28. Degree of nonlinearity

  29. Degree of Nonlinearity DNis determined by the combination of δηprecisely with Hilbert Spectral Analysis. Either of them equals zero means linearity. We can determine δand ηseparately: ηcan bedetermined from the instantaneous frequency modulations relative to the mean frequency. δ can be determined from DN with known η. NB: from any IMF, the value of δη cannot be greater than 1. The combination of δ and η gives us not only the Degree of Nonlinearity, but also some indications of the basic properties of the controlling Differential Equation, the Order of Nonlinearity.

  30. Stokes Models

  31. Data and IFs : C1

  32. Summary Stokes I

  33. Lorenz Model Lorenz is highly nonlinear; it is the model equation that initiated chaotic studies. Again it has three parameters. We decided to fix two and varying only one. There is no small perturbation parameter. We will present the results for ρ=28, the classic chaotic case.

  34. Phase Diagram for ro=28

  35. X-Component DN1=0.5147 CDN=0.5027

  36. Data and IF

  37. Comparisons

  38. How to define and determine Trend ? Parametric or Non-parametric? Intrinsic vs. extrinsic approach?

  39. The State-of-the arts: Trend“One economist’s trend is another economist’s cycle”Watson : Engle, R. F. and Granger, C. W. J. 1991 Long-run Economic Relationships. Cambridge University Press.

  40. PhilosophicalProblem Anticipated 名不正則言不順 言不順則事不成 ——孔夫子

  41. Definition of the TrendProceeding Royal Society of London, 1998Proceedings of National Academy of Science, 2007 Within the given data span, the trend is an intrinsically fitted monotonic function, or a function in which there can be at most one extremum. The trend should be an intrinsic and local property of the data; it is determined by the same mechanisms that generate the data. Being local, it has to associate with a local length scale, and be valid only within that length span, and be part of a full wave length. The method determining the trend should be intrinsic. Being intrinsic, the method for defining the trend has to be adaptive. All traditional trend determination methods are extrinsic.

  42. Algorithm for Trend • Trend should be defined neither parametrically nor non-parametrically. • It should be the residual obtained by removing cycles of all time scales from the data intrinsically. • Through EMD.

  43. Global Temperature Anomaly Annual Data from 1856 to 2003

  44. GSTA

  45. IMF Mean of 10 Sifts : CC(1000, I)

  46. Statistical Significance Test

  47. IPCC Global Mean Temperature Trend

  48. Comparison between non-linear rate with multi-rate of IPCC Blue shadow and blue line are the warming rate of non-linear trend. Magenta shadow and magenta line are the rate of combination of non-linear trend and AMO-like components. Dashed lines are IPCC rates.

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