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Bessel functions

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Journal Article
Published: 06 December 2022
Bulletin of the Seismological Society of America (2023) 113 (1): 361–377.
.... , 2022 ), the f‐k method ( Nishida et al. , 2008 ), and the frequency–Bessel (F–J) transform method ( Wang et al. , 2019 ). Except for the F–J transform method, these methods use the exponential function as part of the integral kernel, thereby implying a plane‐wave assumption ( Wang et al. , 2019...
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Journal Article
Published: 24 June 2022
Bulletin of the Seismological Society of America (2022) 112 (5): 2257–2279.
...Song Luo; Shaoqian Hu; Guili Zhou; Huajian Yao ABSTRACT The frequency–Bessel (F–J) transformation method is effective for the extraction of multimode surface wave dispersion data from ambient noise cross‐correlation functions (CCFs). Recently, this method has been improved in terms of increasing...
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An example of fitting the Bessel functions of the first kind of order zero to the spatial autocorrelation coefficient. The black solid line indicates the Bessel function of best fit to the coefficient. The black circles and error bars indicate the average values at each distance and their standard deviations.
Published: 13 May 2024
Figure 5. An example of fitting the Bessel functions of the first kind of order zero to the spatial autocorrelation coefficient. The black solid line indicates the Bessel function of best fit to the coefficient. The black circles and error bars indicate the average values at each distance
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An example of fitting the first kind of zero‐order Bessel functions to the spatial autocorrelation coefficient at site F16‐1. Solid line, the Bessel function of best fit to the coefficient; open circles with vertical bars, the average and standard deviation values at each distance.
Published: 01 November 2013
Figure 4. An example of fitting the first kind of zero‐order Bessel functions to the spatial autocorrelation coefficient at site F16‐1. Solid line, the Bessel function of best fit to the coefficient; open circles with vertical bars, the average and standard deviation values at each distance.
Image
Difference between (a) the (nondamped) Bessel functions and the real parts of γ(r,ω) and (b) the damped Bessel functions that best fit the real parts γ(r,ω) and these real parts itself. Whitened complex coherencies and models for the 0.20–0.40 Hz vertical component data are shown. The models as well as the real parts of γ(r,ω) are normalized with respect to the proportionality factor A before the differences are calculated. The difference between the model and the data in (a) can be associated with attenuation due to the medium. The cross sections associated with the dashed black lines at 0.25 and 2.00 Hz are shown in Figures 9 and 10, respectively. The triangles on the color bar indicate that the maximum and minimum values are off the scale.
Published: 11 December 2012
Figure 11. Difference between (a) the (nondamped) Bessel functions and the real parts of γ ( r , ω ) and (b) the damped Bessel functions that best fit the real parts γ ( r , ω ) and these real parts itself. Whitened complex coherencies and models for the 0.20–0.40 Hz
Image
Dispersion curves for model 1 using (a) the original Bessel function and (b) the renormalized Bessel function. The black block is caused by an error in root searching using the bisection method in which the imaginary component of Bessel frequently fluctuates near zero.
Published: 27 March 2024
Figure 3. Dispersion curves for model 1 using (a) the original Bessel function and (b) the renormalized Bessel function. The black block is caused by an error in root searching using the bisection method in which the imaginary component of Bessel frequently fluctuates near zero.
Book Chapter

Series: Society of Exploration Geophysicists Geophysical References Series
Published: 01 January 1999
DOI: 10.1190/1.9781560801825.ch7
EISBN: 9781560801825
... complicate things substantially. This chapter demonstrates that problems involving point sources are almost always more easily analyzed in terms of a different sort of basic function, called Bessel functions. Hankel transforms (which use Bessel functions) are introduced, using a modernized version...
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Examples of the Bessel function fitted to the SPAC coefficients at ATS for some representative frequencies. The solid lines show fitted Bessel function and circles and the error bars indicate the means of SPAC coefficients and their standard deviations determined using 20 and 40 time blocks, respectively.
Published: 01 February 2002
Figure 6. Examples of the Bessel function fitted to the SPAC coefficients at ATS for some representative frequencies. The solid lines show fitted Bessel function and circles and the error bars indicate the means of SPAC coefficients and their standard deviations determined using 20 and 40 time
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Comparison of the distribution of imaginary components of the original and renormalized Bessel functions if the wavenumber is 200 m−1 in model 1. Model parameters are provided in Tables 1 and 2. Distribution of the imaginary components of (a) the original Bessel function and (b) the renormalized Bessel function.
Published: 27 March 2024
Figure 2. Comparison of the distribution of imaginary components of the original and renormalized Bessel functions if the wavenumber is 200 m −1 in model 1. Model parameters are provided in Tables  1 and 2 . Distribution of the imaginary components of (a) the original Bessel function and (b
Book Chapter

Series: Society of Exploration Geophysicists Geophysical References Series
Published: 01 January 1999
DOI: 10.1190/1.9781560801825.ch9
EISBN: 9781560801825
... an old calculus in a new calculus. Invariance of mathematical form implies the structure of tensor analysis, and that structure implies the Bessel functions of the previous two chapters; they were just the offset-dependent part of a set of invariants that satisfied the wave equation. In this chapter we...
Journal Article
Journal: Geophysics
Published: 11 December 2012
Geophysics (2013) 78 (1): Q1–Q14.
...Figure 11. Difference between (a) the (nondamped) Bessel functions and the real parts of γ ( r , ω ) and (b) the damped Bessel functions that best fit the real parts γ ( r , ω ) and these real parts itself. Whitened complex coherencies and models for the 0.20–0.40 Hz...
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Journal Article
Published: 01 October 1984
Bulletin of the Seismological Society of America (1984) 74 (5): 1555–1578.
... details affect efficiency and accuracy when synthesizing high-frequency seismograms by multi-mode summation of dispersed surface waves. Avoid branch-line integrals and spherical Bessel functions of nonintegral order by using spherical structures combined with transformations permitting replacement...
Journal Article
Journal: Geophysics
Published: 01 December 1987
Geophysics (1987) 52 (12): 1631–1638.
.... In this process we use the asymptotic approximation for the zeroth-order Bessel function. This approximation reduces the number of computations significantly, but it is valid only for omega px greater than 2 or 3. Using this approximation, we have been able to obtain the correct plane-wave decomposition...
Image
Frequency–Bessel (F‐J) spectra of Green’s functions with different transform methods. (a) Transform with the Bessel function. (b) Transform with the Hankel function. (c) The second part of the transformation with the Hankel function. (d) Our modified transformation. The color version of this figure is available only in the electronic edition.
Published: 31 August 2021
Figure 2. Frequency–Bessel (F‐J) spectra of Green’s functions with different transform methods. (a) Transform with the Bessel function. (b) Transform with the Hankel function. (c) The second part of the transformation with the Hankel function. (d) Our modified transformation. The color version
Journal Article
Journal: Geophysics
Published: 01 February 1983
Geophysics (1983) 48 (2): 224–228.
...A. Soto; S. K. Singh; C. Flores Abstract Expressions for the spectra of gravity and magnetic anomalies due to a vertical right circular cylinder can be written in terms of a Bessel function and the sum of two exponentials. From the zeros of the amplitude spectra, which are the zeros of the Bessel...
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Example of spatial autocorrelation and phase-velocity images at the Manhattan Beach site. The left side of the figure shows the low-frequency component which reflects S-wave velocity structure down to several kilometers, whereas the right side shows the high-frequency component reflecting velocity structure less than about 100 m. (a) Examples of frequency-dependent coherences comparing larger sensor spacing (left) and smaller spacing (right). (b) Typical coherences as a function of sensor distance with theoretical Bessel functions calculated for phase velocities that yield minimum error between the observed coherences and the theoretical Bessel function. The symbols indicate observed coherences and solid lines indicate the theoretical Bessel functions. (c) Error between observed coherences and theoretical Bessel functions with magenta indicating large error and blue indicating small error. Red dots indicate minimum-error phase velocities at each frequency and they can be considered as the observed dispersion curves.
Published: 01 June 2013
reflecting velocity structure less than about 100 m. (a) Examples of frequency-dependent coherences comparing larger sensor spacing (left) and smaller spacing (right). (b) Typical coherences as a function of sensor distance with theoretical Bessel functions calculated for phase velocities that yield minimum
Journal Article
Published: 31 August 2021
Bulletin of the Seismological Society of America (2022) 112 (1): 143–152.
...Figure 2. Frequency–Bessel (F‐J) spectra of Green’s functions with different transform methods. (a) Transform with the Bessel function. (b) Transform with the Hankel function. (c) The second part of the transformation with the Hankel function. (d) Our modified transformation. The color version...
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Journal Article
Published: 01 September 1996
Russ. Geol. Geophys. (1996) 37 (9): 23–45.
... waves or generalized rays. The integrand in the inverse Fourier–Bessel transform of a generalized ray can be expressed as an amplitude and a delay which are functions of slowness only. The inverse Fourier transform of the Bessel function is evaluated analytically. The resulting slowness integral, which...
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Journal Article
Journal: Geophysics
Published: 01 October 1990
Geophysics (1990) 55 (10): 1380–1385.
... along the horizontal slowness axis. This property permits to expand the Hankel transform into a Fourier-Bessel series. In practice, this algorithm requires an interpolation in distance of the recorded dataset, but allows a considerable reduction of Bessel functions calculations. Numerical applications...
Journal Article
Journal: Geophysics
Published: 01 December 1983
Geophysics (1983) 48 (12): 1671–1686.
...Alan D. Chave Abstract An algorithm for the accurate evaluation of Hankel (or Bessel) transforms of algebraically related kernel functions. The algorithm performs the automatic integration of the product of the kernel and Bessel functions between the asymptotic zero crossings of the latter and sums...