Mapping of channel facies revealed three orientations of fill heterogeneity expressed as: (1) upward variations in the character of vertically stacked fill sequences, (2) lateral variability, and (3) the occurrence of downstream dipping and stacking units forming the uppermost parts of channel fill.
Because glycemic fluctuations as estimated from MAGE indexes reflect both upward and downward glucose changes, whereas postprandial values are only markers of upward variations, there is some reason to think that MAGE indexes are wider integrators of glycemic variations than postprandial glucose.
Because the glycemic fluctuations as estimated from MAGE indexes reflect both upward and downward glucose changes, whereas A1C, PPG, and FPG values are only markers of upward variations, there is a reason to hypothesize that MAGE indexes are wider integrators of glycemic variations than the A1C, PPG, and FPG values.
However, the upward sedimentologic variation in the Atacama Gravels evidences a progressive aridification of the climate.
The upward glycemic variation during the night was only considered a dawn phenomenon if its magnitude was above the stochastic spontaneous glucose fluctuations during the early morning period after an overnight fast.
When scores conferred by single courses were compared over time, three time-trend patterns emerged: low variation, upward trend and erratic pattern.
While the overall trend is upward, there remains considerable variation among classes.
Typical results of the variation of upward movement with time for different pile spacing and L/D ratios 27, 35 and 53 are shown in Figs. 22, 23, 24, 25, 26, 27, 28, 29, 30, 31, 32 and 33.
Following to a conceptual problem of the vertically upward flow with quality variation, the small bottom break of a pressurized horizontal pipe is simulated and discussed in some detail.
Yet the economists who did the study do not list race as one of the main factors that explains the variation in upward-mobility rates across regions.
Some part of the resonant wave leaks upward and generates ionospheric variations at these resonant frequencies (Shinagawa et al., 2007).
