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The latest change in the convergence mode is thought to have occurred around 1 ~ 2 Ma.
Similarly, it can be noticed that the fastest convergence mode is obtained when the function from (76) reaches its minimum.
Thus, the present convergence mode between the Eurasian/Philippine Sea plates (Figure 10d) is regarded as the latest temporal fluctuation.
Neglecting the regularization constant (i.e., δ≈0), the fastest convergence mode is achieved for α≈1, which is a well-known result [1, 11, 12].
First, it can be noticed that the performance of the regular NLMS algorithm can be controlled in terms of both parameters, α and δ, either by setting the fastest convergence mode (i.e., α=1) and adjusting the value of δ, or by neglecting the regularization constant (i.e., δ=0) and tuning the value of α.
Finally, loop handling was in "iterate until convergence" mode, since the absence of positive feedback loops in the MAPK pathway and FC representation of the node values ensure that the algorithm will converge.
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Proper orthogonal decomposition was developed to extract the main pressure distributions so that the positions where energy converges can be found and the convergence modes can be recognized.
Combined with the experiments, numerical simulations were conducted to reveal the convergence modes and mechanisms.
It's shown that the proper orthogonal decomposition is a simple and efficient method to identify the convergence modes and find the convergence positions.
It's also found that though detonation strength (knock intensity) can be changed by both equivalence ratios and initial pressures, only the equivalence ratios can change the convergence modes while the initial pressures cannot.
In other words, spatial/temporal variations in sedimentary basin morphology on an active margin give clues to changes in the convergence modes of oceanic plates and to regional tectonic history.
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