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The likelihood pdf is assumed unknown and is estimated by using kernel density estimator at the receiver.
At each scale for each pair of geomagnetic events, the response function is estimated by using the Huber M-estimator described by Chave et al.
The scale-W parameter is estimated by using the maximum likelihood estimator (MLE) method and assuming that the shape parameter is known.
(ii) The noiseless part is estimated by using (47).
Bank size is estimated by using total assets.
(i) The noise part is estimated by using (45).
The MSC is estimated by using Welch's averaged periodogram method.
Trophic state index is estimated by using Eqs.
The noiseless part is estimated by using (47).
The sensing performance is estimated by using dispersion diagram through using plane wave expansion simulations.
At first, the conducted emission of the DC is estimated by using the ICEM-CE model.
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