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The correlation between MOS-LQS and MOS-LQO samples is computed using Pearson's formula (2).
The ETC of the samples is computed using the finite volume method (FVM) on the basis of 3D multi-mode heat transfer simulation.
A moving window with the length of half cycle of power frequency is considered and the RMS value of the current samples is computed in the window.
The distance between two samples is computed using the Pearson Correlation based distance (5).
In our metric, the distance between sets of variants from two exome samples is computed without considering genotyping quality scores.
The average of the class ('C1'.....CM..'.....CM') samples is computed as (1) where N ω is the number of exemplars of class ω, and x iω is the feature vector of the ith exemplar of class ω.
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Chroma samples are computed using four-tap filters.
Chroma samples are computed by the weighed interpolation of four closest integer pixel samples.
The time domain samples are computed using the well-known IFFT formula (1).
Salinity index of the groundwater samples were computed using the measured EC values.
CVA concentrations in the spiked RLM samples were computed by substituting their ratios into the generated linear regression equation.
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