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Here, we simulated the long-period ground motions using the estimated source model and 1-D velocity structure models.
Finally, using the estimated source model together with the 1-D velocity structure model for the Kathmandu basin, we carried out the waveform simulation of long-period (> 4 s) ground motions at a site located in the Kathmandu basin.
Using the estimated source model together with the 1-D velocity structure model of the Kathmandu basin, we simulated the long-period (> 4 s) ground motions at KATNP located in the Kathmandu basin.
Using the estimated source model together with a one-dimensional (1-D) velocity basin structure model, long-period (> 4 s) ground motions were simulated at a site located in the Kathmandu basin, where strong ground motions with predominant components in a 4 5s period were observed during the 2015 Gorkha earthquake.
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Then, the speaker-to-speaker ratio is assessed using the estimated sources.
To assign vocal signals to specific mice, we used the estimated source position in combination with the location of the mice at the time of the vocal signal and a confidence measure in the estimated source position.
The estimated source location using the BLUE estimator is shown in Figure 4 as a function of the number of nodes and time samples for different values of σ m 2 s.
In Sections 3 and 4, we present the technique using the estimated multicomponent wideband spectral matrices of sources leading to the estimations of the polarization and of the DOA parameters for each wavefield.
In the following, we propose a method to estimate the ranges and DOA of the sources by using the estimated TDOA of the received signals on the different sensors.
Then, the estimated sources are used to predict tsunami arrival times and the amplitudes at more distant locations.
The algorithm is an extension of the Infomax BSS system for which a measure of distance between a carefully measured P300 and the estimated sources is used as a constraint.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com