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Fortunately, it turns out that the achieved feature extraction (i.e., rank reduction) with only local minima has been shown to be of significant quality for many applications [55].
However, their values can be favorably compared with the results presented for these quantities in the work of Lima et al. [41], where the minima has been obtained by choosing a parameter that enforces that behavior.
For 13 ≤ n ≤ 20, an unbiased search for the global minima has been undertaken based on either the genetic algorithm coupled with semi-empirical tight-binding (TB) technique [17] or the single-parent evolution algorithm coupled with density functional (DF), TB, and density functional theory (DFT) methods [18, 19].
These figures demonstrate that in the case of minimum-phase channel there is almost no chance of converging to local minima, while in the case of nonminimum phase channels a 5 10percentt of convergence to local minima has been detected.
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Sixteen minima have been found on the potential energy surface.
(c) shows pixels where the steepest descending paths and minima have been labelled.
Chemisorption barrier and partial charge transfer to the metal for transition between the two potential minima have been examined and compared with experimental data.
A total of 22 local minima have been located by geometry optimization of 216 possible trial structures at the B3LYP/6-31+G* B3LYP/6-31+G*ry.
Earlier extended minima have been discovered through analysis of tree rings and appear to have coincided with lower-than-average global temperatures.
Various methods based on monotone minimum, linear interpolation and moving average of minima have been utilized in baseline estimation [ 9, 11].
Since 1978, when direct satellite measurements of sea ice started, the average summertime minimum has been 2.4 million square miles.
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