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To evaluate the dependence of the duration of source time function on the amplitude level variance, we conducted FDM simulations using different sin waves, which had 1, 2, 3, 6, and 9 s durations (no. 2 6 source time functions).
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The amplitude level variance in the weak wavefield fluctuation regime was very similar among the different durations of source time function (Fig. 10a); however, the values in the strong wavefield fluctuation regime increased with the decreasing duration of the source time function.
The FDM simulations in this study demonstrated that variations of wave amplitude in random inhomogeneous media depend on not only the inhomogeneity of the medium but also on the duration of the source wavelet.
(20 2)sualize and interpret the spatial and temporal distributions of both the water height and the velocity vector in the sea from the sea-bottom deformation including, in particular, the finite duration of the source process time.
However, in the strong wavefield fluctuation regime, the amplitude level variance was larger for the Ricker wavelet than that for quasi-time-harmonic waves; therefore, amplitude fluctuations may depend on the duration of the source wavelet.
The moment tensor inversion (Fig. 4) supports this idea, although the centroid depth of the 2014 Fukushima-oki earthquake cannot be as sharply determined as for the 2012 event because the 2014 event has a shorter duration of the source time function.
We consider a slow fading environment with a finite coherence time that is longer than the duration of the source phase and the relay phase, so that the fading gain between two network nodes takes the same value during both phases.
Although coal-fired municipal furnaces and industrial activity are most likely to be the main source of the outdoor PAHs (Lvovsky et al. 2000), we could not determine the exact extent and duration of these sources during our air-monitoring campaign.
Moment analysis of the nonwetting phase showed that large-scale movement had ceased after approximately 9 years (maximum duration of the source-on condition was approximately 4.5 years).
In Fig. 4, we show the distribution of waveform variance as a function of the half-duration of the source time function (Tr) and the centroid depth.
Moment tensor solutions colored based on their variance as a function of the half-duration of the source time function (Tr) and the centroid depth.
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