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The MLE algorithm was modified from the Newton Raphson method (Tanner, 1996), to prevent the estimates for the model in Equation (2) being trapped in local maxima, which was caused by the sinusoidal functions in the joint density.
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The obtained I-t transients exhibit current maxima which are analyzed for the nucleation type.
Particular emphasis is placed on the viscous stresses and their local maxima, which are analyzed and discussed in detail.
Background color indicates correlation of glacial and interglacial maxima, which are defined by benthic δ18O measurements and TWC indicators, respectively.
Only those local maxima which are higher than a threshold (i.e. ρ t, f) > 0.01 × max(ρ t, f))) are considered as valid peaks.
On the other hand, when they do not have any expectations, they explain the graph based on minima and maxima which are in line with the present study.
Then, the pseudo spectrum of α may have P local maxima which are denoted as (left { {{{hat alpha }_{1}}, cdots,{{hat alpha }_{P}}} right }).
So, we can sum up these two phases in only one phase by considering maxima, which are greater than a threshold θ.
We observe two pronounced maxima, which are attributed to the values of a for the developing phases.
Simulations further indicate the presence of two adsorption maxima, which are located at φ = 12° and −48°.
One problem with the implementation of LRTs is the existence of suboptimal local maxima, which is overcome by use of several different starting points for the likelihood maximization.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com