Abstract

Magnetotelluric (MT) data consist of the sum of several types of natural sources including transient and quasiperiodic signals and noise sources (instrumental, anthropogenic) whose nature has to be taken into account in MT data processing. Most processing techniques are based on a Fourier transform of MT time series, and robust statistics at a fixed frequency are used to compute the MT response functions, but only a few take into account the nature of the sources. Moreover, to reduce the influence of noise in the inversion of the response functions, one often sets up another MT station called a remote station. However, even careful setup of this remote station cannot prevent its failure in some cases. Here, we propose the use of the continuous wavelet transform on magnetotelluric time series to reduce the influence of noise even for single site processing. We use two different types of wavelets, Cauchy and Morlet, according to the shape of observed geomagnetic events. We show that by using wavelet coefficients at clearly identified geomagnetic events, we are able to recover the unbiased response function obtained through robust remote processing algorithms. This makes it possible to process even single station sites and increase the confidence in data interpretation.

Highlights

  • The magnetotelluric (MT) method is based on the induction of natural electromagnetic (EM) fields in the ground

  • The other main class of EM waves is due to the interaction of the solar wind with the Earth’s magnetic field, and this produces magnetohydrodynamic waves that are transmitted in the atmosphere through the ionosphere from the magnetosphere (Saito 1969; McPherson 2005)

  • We demonstrate that the continuous wavelet transform (CWT) may be a powerful tool to reduce the bias in the computation of the impedance tensor, even in the case of single station processing

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Summary

Introduction

The magnetotelluric (MT) method is based on the induction of natural electromagnetic (EM) fields in the ground. The MT method is based on the quasi-uniform source assumption whereby sources are supposed to be far from the measurement point (Chave and Jones 2012, Chapter 2). In this approximation, the horizontal electric field e = (ex, ey) is linked to the horizontal magnetic field h = (hx, hy) by convolution products ∗ (in the time domain) with impulse response functions (zxx, zxy , zyx, and zyy), which are components of the impedance tensor z: ex(t) = zxx(t) ∗ hx(t) + zxy(t) ∗ hy(t), ey(t) = zyx(t) ∗ hx(t) + zyy(t) ∗ hy(t)

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