Legendre polynomial-based robust Fourier transformation and its use in reduction to the pole of magnetic data

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Acta Geodaetica et Geophysica Pub Date : 2021-08-16 DOI:10.1007/s40328-021-00357-1
Daniel Oduro Boatey Nuamah, Mihály Dobróka, Péter Vass, Mátyás Krisztián Baracza
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引用次数: 3

Abstract

A new inversion based Fourier transformation technique named as Legendre-Polynomials Least-Squares Fourier Transformation (L-LSQ-FT) and Legendre-Polynomials Iteratively Reweighted Least-Squares Fourier Transformation (L-IRLS-FT) are presented. The introduced L-LSQ-FT algorithm establishes an overdetermined inverse problem from the Fourier transform. The spectrum was approximated by a series expansion limited to a finite number of terms, and the solution of inverse problem, which gives the values of series expansion coefficients, was obtained by the LSQ method. Practically, results from the least square method are responsive to data outliers, thus scattered large errors and the estimated model values may be far from reality. A definitely better option is attained by introducing Steiner’s Most Frequent Value method. By combining the IRLS algorithm with Cauchy-Steiner weights, the Fourier transformation process was robustified to give the L-IRLS-FT method. In both cases Legendre polynomials were applied as basis functions. Thus the approximation of the continuous Fourier spectra is given by a finite series of Legendre polynomials and their coefficients. The series expansion coefficients were obtained as a solution to an overdetermined non-linear inverse problem. The traditional DFT and the L-IRLS-FT were tested numerically using synthetic datasets as well as field magnetic data. The resulting images clearly show the reduced sensitivity of the newly developed L-IRLS-FT methods to outliers and scattered noise compared to the traditional DFT. Conclusively, the newly developed L-IRLS-FT can be considered to be a better alternative to the traditional DFT.

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基于勒让德多项式的鲁棒傅里叶变换及其在磁数据极点化约中的应用
提出了一种新的基于反演的傅里叶变换技术,即legende多项式最小二乘傅里叶变换(L-LSQ-FT)和legende多项式迭代重加权最小二乘傅里叶变换(L-IRLS-FT)。引入的L-LSQ-FT算法从傅里叶变换出发建立了一个过定反问题。用有限项的级数展开来逼近谱,用LSQ方法得到了给出级数展开系数值的反问题解。在实际应用中,最小二乘法的结果对数据异常值的响应较大,误差较大,估计的模型值可能与实际情况相差较大。一个更好的选择是通过引入斯坦纳最常值法。将IRLS算法与Cauchy-Steiner权值相结合,对傅里叶变换过程进行鲁棒化,得到L-IRLS-FT方法。在这两种情况下,勒让德多项式都被用作基函数。因此,连续傅立叶谱的近似是由有限列的勒让德多项式及其系数给出的。得到了一类超定非线性逆问题的级数展开系数。利用合成数据集和磁场数据对传统DFT和L-IRLS-FT进行了数值测试。结果显示,与传统的DFT相比,新开发的L-IRLS-FT方法对异常值和散射噪声的灵敏度降低。总之,新开发的L-IRLS-FT可以被认为是传统DFT的更好选择。
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来源期刊
Acta Geodaetica et Geophysica
Acta Geodaetica et Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.10
自引率
7.10%
发文量
26
期刊介绍: The journal publishes original research papers in the field of geodesy and geophysics under headings: aeronomy and space physics, electromagnetic studies, geodesy and gravimetry, geodynamics, geomathematics, rock physics, seismology, solid earth physics, history. Papers dealing with problems of the Carpathian region and its surroundings are preferred. Similarly, papers on topics traditionally covered by Hungarian geodesists and geophysicists (e.g. robust estimations, geoid, EM properties of the Earth’s crust, geomagnetic pulsations and seismological risk) are especially welcome.
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