The primary amplitude measure of pressure pulsatility is the absolute pulse amplitude, that is, the nadir-to-peak variation in pressure.
This mechanism explains the high PL peak variation found in squalane (−0.91 meV/K).
The 2D peak variation originates in that the three effective sub-modes correlate with the light polarization through different relations.
Seasonal adjusted factor showed peak seasonal variation in the second quarter (April–June).
The measured and simulated profiles showed reasonable agreement in shape, peak location, emission zone thickness, and peak-intensity variation in fuel-lean and stoichiometric flames.
For example, Stergiou et al 12 demonstrated that the two-peak diurnal variation in stroke onset occurs in parallel with variation in blood pressure, pulse rate and physical activity.
Our previous study in Hong Kong also found a two-peak seasonal variation in mortality burden of influenza, which is similar to the pattern of influenza seasonality, suggesting that environmental factors might also affect the severity of seasonal influenza infection [ 16].
For instance, large numbers of distinct variants in the pool increase the likelihood of overlapping, indistinguishable peaks, or variation in the gel matrix between runs confounds the comparison of samples that have been run at different times.
The DSC thermograms of the prepared solvates showed a single broad endothermic peak with slight variation in onset temperatures followed by not so sharp melting endotherms.
The peaks with low variation in log (read count + 1) within ±50 bp from the MACS summit are considered constitutive.
The previous observations suggest that the size distribution of the pores correlated qualitatively with the intensities and the positions of the PL peaks, whereas variations in the chemical composition at the surface show no systematic correlation [39, 40].
