In mixtures of four organoclays with the two polymers, WAXS (wide angle X-ray scattering) peak height and shift in gallery height was the same for a given organoclay.
The arrow and bars in C illustrate the shift in boundary height between high (bottom bar) and low (top bar) go trial probability conditions.
In general, mesospheric echoes show tilted layers, a sporadic nature above/below the main layer (70 80 km), and a seasonal shift in the height of occurrence.
Fig. 1 Typical range-time Signal-to-Noise Ratio (SNR) contours showing (a) descending layers, (b) patchy layers above/below the main layer, and (c) echoes showing a seasonal shift in the height of occurrence observed in different seasons.
Differences in their gain caused a shift in pulse height spectra and were corrected by using individually adjusted high voltage supplies to the two PMTs (1,165 and 985 V).
The acoustic changes triggered by the F0 context also do not affect all formants at all points in time in the same way (e.g. in the same direction) as it would be the case if segmental intonation was caused by a F0-related shift in larynx height.
However, for some languages and intonational or tonal embeddings, studies failed to find segmental intonation, which is one of the reasons why a general articulatory mechanism of pitch change, such as a shift in larynx height (cf. Coleman et al. [93]), is not a likely explanation for the parallel between the pitch impressions of fricatives and their adjacent F0 contexts.
Increasing free Ca2+ up to 0.06 µM caused a slight increase in peak height, while its further increase led to a fall in peak height, and a shift in peak fluorescence to around 337 nm (see Figure 3A,B).
The acoustic changes associated with segmental intonation are much larger (formants move upward or downward by up to 66%) than those that would be expected from F0-related shifts in larynx height.
As a result of these changes flying at higher altitude results in a change in the distribution of echo categories, an upward shift in the canopy-height distribution and a lower proportion of multiple returns (Goodwin et al. 2006; Næsset 2004b, 2009).
