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Chroma samples are computed using four-tap filters.
The time domain samples are computed using the well-known IFFT formula (1).
Chroma samples are computed by the weighed interpolation of four closest integer pixel samples.
This data flow cannot be applied directly in HEVC since the quarter-pel samples are computed using separate filters.
We compare MCAP results with those offered by the classical AP approach (Frey and Dueck, 2007), where the similarities (negative distances) between the samples are computed as negative squared error distances (Frey and Dueck, 2007).
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The ETC of the samples is computed using the finite volume method (FVM) on the basis of 3D multi-mode heat transfer simulation.
As a final result, when the simulated distribution in 10 kg samples was computed from the prior simulation, it was very similar to the distribution observed in representative samples for the same sample size from the RASFF.
The correlation between MOS-LQS and MOS-LQO samples is computed using Pearson's formula (2).
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.
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.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com