scholarly journals A New Way of Understanding why the Harmonic Series is Divergent

Keyword(s):  
2003 ◽  
Vol 128 (1) ◽  
pp. 71-97
Author(s):  
Chris Collins

This article challenges two tenets of Falla scholarship: that the composer made use of a system of chord generation based on the harmonic series, and that he learnt this technique from Louis Lucas's L'acoustique nouvelle (Paris, 1854). The author demonstrates that Lucas's theories are largely unconcerned with the harmonic series and that Falla's use of ‘natural resonance’ has been misunderstood. Study of Falla's work, including manuscripts and writings (published and unpublished), reveals the true nature of Lucas's influence. Consideration is also given to Falla's role in the creation of this false orthodoxy.


2020 ◽  
Vol 94 (9) ◽  
Author(s):  
Lars E. Sjöberg

Abstract As the KTH method for geoid determination by combining Stokes integration of gravity data in a spherical cap around the computation point and a series of spherical harmonics suffers from a bias due to truncation of the data sets, this method is based on minimizing the global mean square error (MSE) of the estimator. However, if the harmonic series is increased to a sufficiently high degree, the truncation error can be considered as negligible, and the optimization based on the local variance of the geoid estimator makes fair sense. Such unbiased types of estimators, derived in this article, have the advantage to the MSE solutions not to rely on the imperfectly known gravity signal degree variances, but only the local error covariance matrices of the observables come to play. Obviously, the geoid solution defined by the local least variance is generally superior to the solution based on the global MSE. It is also shown, at least theoretically, that the unbiased geoid solutions based on the KTH method and remove–compute–restore technique with modification of Stokes formula are the same.


1966 ◽  
Vol 44 (5) ◽  
pp. 987-994 ◽  
Author(s):  
R. E. Barrington ◽  
Luise Herzberg

Ionograms produced by the Alouette I topside sounder frequently show well-developed series of cyclotron harmonics. Their frequencies have been determined from A (amplitude) scans with an accuracy of ~0.02 Mc/s for the sweep range of 1 to 6 Mc/s. In all cases examined, the frequencies of all of the members of the harmonic series are, within the experimental accuracy, integral multiples of the cyclotron frequency derived from the best present estimates of the earth's magnetic field strength at the satellite height. This result is discussed in the light of recent laboratory results and theoretical studies.


2007 ◽  
Vol 64 (11) ◽  
pp. 4098-4112 ◽  
Author(s):  
Haruma Ishida ◽  
Shoji Asano

Abstract A new calculation scheme is proposed for the explicitly discretized solution of the three-dimensional (3D) radiation transfer equation (RTE) for inhomogeneous atmospheres. To separate the independent variables involved in the 3D RTE approach, the spherical harmonic series expansion was used to discretize the terms, depending on the direction of the radiance, and the finite-volume method was applied to discretize the terms, depending on the spatial coordinates. A bidirectional upwind difference scheme, which is a specialized scheme for the discretization of the partial differential terms in the spherical harmonic-transformed RTE, was developed to make the equation determinate. The 3D RTE can be formulated as a simultaneous linear equation, which is expressed in the form of a vector–matrix equation with a sparse matrix. The successive overrelaxation method was applied to solve this equation. Radiative transfer calculations of the solar radiation in two-dimensional cloud models have shown that this method can properly simulate the radiation field in inhomogeneous clouds. A comparison of the results obtained using this method with those using the Monte Carlo method shows reasonable agreement for the upward flux, the total downward flux, and the intensities of radiance.


1994 ◽  
Vol 72 (7-8) ◽  
pp. 505-510 ◽  
Author(s):  
D. J. Rowe

We review the properties of the holomorphic representations with lowest weights for the noncompact real symplectic and metaplectic groups. The unitarizable sub representations of these representations are identified with the harmonic series. We define unitary characters for the holomorphic representations and show how they can be used to identify the unitarizable sub quotient representations. Explicit results are given for Sp(1, R), Sp(2, R), and Sp(3, R).


In a paper contributed to the Hann celebration volume of the Meteorologische Zeitschrift , I endeavoured to account for a curious relation between the yields of wheat for successive years in the eastern district of England by referring the variation to periodic components. The relation referred to will be understood from an inspection of the table of yields on p. 75, or the diagram which illustrates it. The yields for the years 1896, 1897, and so on, taken in chronological order, apparently “compensate” respectively those for 1895, 1894, and so on, taken in reversed chronological order. Each pair of years at equal intervals, one before and one after 1895—6, gives a mean value approximating very closely to 30.8 bushels per acre, the average yield for the 20 years 1885 to 1904. This relation is further illus­trated by the yield for 1905, which was not ascertained when the paper referred to was written (November, 1905). The data have been issued since then by the Board of Agriculture, and the yield for 1905 comes out at 32.0 bushels per acre, which “compensates” the yield for 1886, 29·2 bushels per acre, the mean being 30·6, surprisingly near to 30·8. The work of the paper referred to was based upon the supposition that a reversal of the kind indicated points to the yield being represented by the combination of a number of simple harmonic components, each having a node, ascending or descending, at the epoch 1895—6. At first I did not suppose that the components belonged to a harmonic series, and I tried to evaluate them by eliminating components of specified period, two years, four years, etc., by numerical process. The simplification produced by taking the mean of consecutive years, and thus eliminating the simple periodic term of two years’ period was considerable, and, in my contribution to the “Hann” volume, I dealt with the curve thus simplified. When I had selected periodic terms to give the best representation I could make of the curve of two-year means, one of the terms had a period of 11 years, and I could draw no practical distinction between the others and the harmonic components of a fundamental period of 11 years. In the result it was shown that the average yield for two consecutive year' yield of wheat in the eastern counties of England between 1885 and 1904 was represented with remarkable fidelity by the equation y = 31+2·8 sin 2π/11 n + 0·4 sin 4π/11 n - 1·2 sin 6π/11 n + 1·2 sin 8π/11 n , where n is the number of years, counting backwards or forwards, from the point representing the mean for 1895—6.


2019 ◽  
Author(s):  
John Mcbride ◽  
Tsvi Tlusty

Musical scales are used throughout the world, but the question of how they evolved remains open. Some suggest that scales based on the harmonic series are inherently pleasant, while others propose that scales are chosen that are easy to communicate.However, testing these theories has been hindered by the sparseness of empirical evidence. Here, we assimilate data from diverse ethnomusicological sources into a cross-cultural database of scales. We generate populations of scales based on multiple theories and assess their similarity to empirical distributions from the database. Most scales tend to include intervals which are close in size to perfect fifths (“imperfect fifths”), and packing arguments explain the salient features of the distributions. Scales are also preferred if their intervals are compressible, which may facilitate efficient communication and memory of melodies. While scales appear to evolve according to various selection pressures, the simplest, imperfect-fifths packing model best fits the empirical data.


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