1. Frequency and Instantaneous Frequency A Totally New View of Frequency

2. Definition of Frequency Given the period of a wave as T ; the frequency is defined as

3. Equivalence : The definition of frequency is equivalent to defining velocity as Velocity = Distance / Time But velocity should be V = dS / dt.

4. Traditional Definition of Frequency frequency = 1/period. Definition too crude Only work for simple sinusoidal waves Does not apply to nonstationary processes Does not work for nonlinear processes Does not satisfy the need for wave equations

5. Definitions of Frequency : 1 For any data from linear Processes

6. Jean-Baptiste-Joseph Fourier 1807 “On the Propagation of Heat in Solid Bodies” 1812 Grand Prize of Paris Institute “Théorie analytique de la chaleur” ‘... the manner in which the author arrives at these equations is not exempt of difficulties and that his analysis to integrate them still leaves something to be desired on the score of generality and even rigor. ’ 1817 Elected to Académie des Sciences 1822 Appointed as Secretary of Académie paper published Fourier’s work is a great mathematical poem. Lord Kelvin

7. Fourier Spectrum

8. Random and Delta Functions

9. Fourier Components : Random Function

10. Fourier Components : Delta Function

12. Problems with Integral methods Frequency is not a function of time within the integral limit; therefore, the frequency variation could not be found in any differential equation, other than a constant. The integral transform pairs suffer the limitation imposed by the uncertainty principle.

13. Definitions of Frequency : 2 For Simple Dynamic System This is an system analysis but not a data analysis method.

14. Definitions of Frequency : 3 Instantaneous Frequency for IMF only

15. Teager Energy Operator : the Idea H. M. Teager, 1980: Some observations on oral air flow during phonation, IEEE Trans. Acoustics, Speech, Signal Processing, ASSP-28-5, 599-601.

16. Generalized Zero-Crossing : By using intervals between all combinations of zero-crossings and extrema. T1T1 T2T2 T4T4

17. Generalized Zero-Crossing : Computing the weighted frequency.

18. Problems with TEO and GZC TEO has super time resolution but it is strictly for linear processes. GZC is robust but its resolution is too crude.

19. Definitions of Frequency : 4 Instantaneous Frequency for IMF only

20. Instantaneous Frequency

21. Instantaneous Frequency is indispensable for nonlinear Processes x

22. The Idea and the need of Instantaneous Frequency According to the classic wave theory, the wave conservation law is based on a gradually changing φ(x,t) such that Therefore, both wave number and frequency must have instantaneous values. But how to find φ(x, t)?

23. Prevailing Views The term, Instantaneous Frequency, should be banished forever from the dictionary of the communication engineer. J. Shekel, 1953 The uncertainty principle makes the concept of an Instantaneous Frequency impossible. K. Gröchennig, 2001

24. Ideal case for Instantaneous Frequency Obtain the analytic signal based on real valued function through Hilbert Transform. Compute the Instantaneous frequency by taking derivative of the phase function from AS. This is true only if the function is an IMF, and its imaginary part of the analytic signal is identical to the quadrature of the real part. Unfortunately, this is true only for very special and simple cases.

25. Hilbert Transform : Definition

26. Limitations for IF computed through Hilbert Transform Data must be expressed in terms of Intrinsic Mode Function. (Note : Traditional applications using band-pass filter distorts the wave form; therefore, it can only be used for linear processes.) IMF is only necessary but not sufficient. Bedrosian Theorem: Hilbert transform of a(t) cos θ(t) might not be exactly a(t) sin θ(t). Spectra of a(t) and cos θ(t) must be disjoint. Nuttall Theorem: Hilbert transform of cos θ(t) might not be sin θ(t) for an arbitrary function of θ(t). Quadrature and Hilbert Transform of arbitrary real functions are not necessarily identical. Therefore, a simple derivative of the phase of the analytic function for an arbitrary function may not work.

27. Data : Hello

30. Empirical Mode Decomposition Sifting to produce IMFs

31. Bedrosian Theorem Let f(x) and g(x) denotes generally complex functions in L 2 (-∞, ∞) of the real variable x. If (1) the Fourier transform F(ω) of f(x) vanished for │ω│> a and the Fourier transform G(ω) of g(x) vanishes for │ω│< a, where a is an arbitrary positive constant, or (2) f(x) and g(x) are analytic (i. e., their real and imaginary parts are Hilbert pairs), then the Hilbert transform of the product of f(x) and g(x) is given H { f(x) g(x) } = f(x) H { g(x) }. Bedrosian, E., 1963: A Product theorem for Hilbert Transform, Proceedings of the IEEE, 51, 868-869.

32. Nuttall Theorem For any function x(t), having a quadrature xq(t), and a Hilbert transform xh(t); then, where Fq(ω) is the spectrum of xq(t). Nuttall, A. H., 1966: On the quadrature approximation to the Hilbert Transform of modulated signal, Proc. IEEE, 54, 1458

33. Difficulties with the Existing Limitations Data are not necessarily IMFs. Even if we use EMD to decompose the data into IMFs. IMF is only necessary but not sufficient because of the following limitations: Bedrosian Theorem adds the requirement of not having strong amplitude modulations. Nuttall Theorem further points out the difference between analytic function and quadrature. The discrepancy, however, is given in term of the quadrature spectrum, which is an unknown quantity. Therefore, it cannot be evaluated. Nuttall Theorem provides a constant limit not a function of time; therefore, it is not very useful for non-stationary processes.

34. Analytic vs. Quadrature X(t) Y(t) Z(t) Analytic Hilbert Transform Q(t) Quadrature, not analytic No Known general method Analytic functions satisfy Cauchy-Reimann equation, but may be x 2 + y 2 ≠ 1. Then the arc-tangent would not recover the true phase function. Quadrature pairs are not analytic, but satisfy strict 90 o phase shift; therefore, x 2 + y 2 = 1, and the arc-tangent always gives the true phase function. For cosθ(t) with arbitrary function of θ(t) :

35. Normalization To overcome the limitation imposed by Bedrosian Theorem

36. Why do we need Decomposition and Normalization : We need a method to reduce the data to Intrinsic Mode Functions; then we also need a method for AM FM decomposition to over come the difficulties stated in Bedrosian Theorem. An Example : Step-function with Carrier

37. Data : Step-function with Carrier

38. Fourier Spectra for Step-function and Carrier

39. Hilbert Spectrum : Step-function with Carrier

40. Morlet Wavelet : Step-function with Carrier

41. Spectrogram : Step-function with Carrier

42. Data : Step-function with Carrier III

43. Hilbert Spectrum : Step-function with Carrier III

44. Problems with Hilbert Transform method If there is any amplitude change, the Fourier Spectra for the envelope and carrier are not separable. Thus, we violated the limitations stated in the Bedrosian Theorem; drastic amplitude change produce drastic deteriorating results. Once we cannot separate the envelope and the carrier, the analytic signal through Hilbert Transform would not give the phase function of the carrier alone without the influence of the variation from the envelope. Therefore, the instantaneous frequency computed through the analytic signal ceases to have full physical meaning; it provides an approximation only.

45. Effects of Normalization Normalization method can give a true AM FM decomposition to over come the difficulties stated in Bedrosian Theorem, and also provide a sharper error index than Nuttall Theorem.

46. NHHT : Procedures Obtain IMF representation of the data from siftings. Find local maxima of the absolute value of IMF (to take advantage of using both upper and lower envelopes) and fix the end values as maxima to ameliorate the end effects. Construct a Spline Envelope (SE) through the maxima. When envelope goes under the data, straight line envelope will be used for that section of the SE. Normalize the data using SE : N-data = Data/SE. This steps can be repeated. Compute IF (FM) and Absolute Value (AV) from Hilbert Transform of N-data. Definition : Error Index = (AV-1) 2. Compute Instantaneous Frequency for SE (AM).

47. NHHT Procedures : 1. IMF from Data through siftings

48. NHHT Procedures : 2. Locate local maxima and fix the ends

49. NHHT Procedures : 3. Construct the Cubic Spline Envelope (CSE)

50. NHHT procedures:

51. NHHT Procedures : 4. Normalize the IMF through CSE

52. NHHT Procedures : 5. Compute IF through Hilbert Transform

53. NHHT Procedures : 6. Comparison of Hilbert Transforms of Data and Normalized data

54. NHHT Procedures : 7. Define the Error Index = (AV – 1) 2.

55. NHHT Procedures : 8. Define the IMF of Envelope

56. NHHT Procedures : 9. AM and FM of y=c3y(7001:8000,9)

57. NHHT : Procedures Obtain IMF representation of the data from siftings. Find local maxima of the absolute value of IMF (to take advantage of using both upper and lower envelopes) and fix the end values as maxima to ameliorate the end effects. Construct a Spline Envelope (SE) through the maxima. When envelope goes under the data, straight line envelope will be used for that section of the SE. Normalize the data using SE : N-data = Data/SE. This steps can be repeated. Compute IF (FM) and Absolute Value (AV) from Hilbert Transform of N-data. Definition : Error Index = (AV-1) 2. Compute Instantaneous Frequency for SE (AM).

58. Example : Exponentially Decaying Cubic Chirp Model function

59. Exponentially decaying cubic chirp : Equation

60. Exponentially decaying cubic chirp : Data

61. Exponentially decaying cubic chirp : Normalizing function

62. Exponentially decaying cubic chirp : Normalized carrier

63. Exponentially decaying cubic chirp : Phase Diagram

64. Exponentially decaying cubic chirp : Instantaneous Frequency

65. Exponentially decaying cubic chirp : Error Indices

66. Quadrature To circumvent the limitation imposed by Nuttall Theorem

67. Nuttall Theorem For any function x(t), having a quadrature xq(t), and a Hilbert transform xh(t); then, where Fq(ω) is the spectrum of xq(t). Nuttall, A. H., 1966: On the quadrature approximation to the Hilbert Transform of modulated signal, Proc. IEEE, 54, 1458

68. Why do we need Quadrature : To over come the difficulties stated in Nuttall Theorem for complicate phase functions. An Example : Duffing Pendulum

69. Duffing : Model Equation

70. Duffing : Expansions of the Model Equation

71. Duffing : Data

72. Duffing : Data, Quadrature & Hilbert

73. Duffing : Amplitude

74. Duffing : Phase

75. Duffing : Frequency truth is given by quadrature

76. Quadrature : Procedures Normalize the IMFs as in the NHHT method. Compute IF (FM) from Quadrature of N-data as follows:

77. Validation of NHHT and Quadrature Methods Through examples using NHHT HHT GZC TEO Quadrature

78. Example : Duffing Equation Model function

79. Damped Chirp Duffing Model

87. Example : Speech Signal ‘ Hello ’ Real Data

88. Data : Hello

89. Data : Hello IMF

90. Hello : Data c3y(8)

91. Hello : Check Bedrosian Theorem

93. Hello : Instantaneous Frequency & data c3y(8)

94. Hello : Instantaneous Frequency & data Details c3y(8)

95. A Physical Example : Water Surface Waves Real Laboratory Data

96. The Idea and the need of Instantaneous Frequency According to the classic wave theory, the wave conservation law is based on a gradually changing φ(x,t) such that Therefore, both wave number and frequency must have instantaneous values.

97. The Idea and the need of Instantaneous Frequency According to the classic wave theory, there are other more important wave conservation laws for Energy and Action: Therefore, if frequency is a function of time, it has to satisfy certain condition for both laws to be valid.

98. Data

99. Governing Equations I:

100. Governing Equations II:

101. Governing Equations III:

102. Governing Equations IV: The 4 th order Nonlinear Schrodinger Equation

103. Dysthe, K. B., 1979: Note on a modification to the nonlinear Schrodinger equation for application to deep water waves. Proc. R. Soc. Lond., 369, 105-114. Equation by perturbation up to 4 th order. But ω = constant.

104. Data and IF : Station #1

105. Data and IF : Station #3

106. Data and IF : Station #5

107. Phase Averaged Data and IF : Station #1

108. Phase Averaged Data and IF : Station #2

109. Phase Averaged Data and IF : Station #3

110. Phase Averaged Data and IF : Station #4

111. Summary Instantaneous frequency could be highly variable with high gradient. The assumption used in the classic wave theory might not be totally attainable. Coupled with the fusion of waves, we might need a new paradigm for water wave studies.

112. Comparisons of Different Methods TEO extremely local but for linear data only. GZC most stable but offers only smoothed frequency over ¼ wave period at most. HHT elegant and detailed, but suffers the limitations of Bedrosian and Nuttall Theorems. NHHT, with Normalized data, overcomes Bedrosian limitation, offers local, stable and detailed Instantaneous frequency and Error Index for nonlinear and nonstationary data. Quadrature is the best, but the sampling rate has to be sufficiently high.

113. Conclusions Instantaneous Frequency could be calculated routinely from the normalized IMFs through quadrature (for high data density) or Hilbert Transform (for low data density). For any signal, there might be more than one IF value at any given time. For data from nonlinear processes, there has to be intra-wave frequency modulations; therefore, the Instantaneous Frequency could be highly variable.