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Wave amplitude is a major determinant of esophageal clearance.
FDRs also had decreased slow wave amplitude and slopes.
When tsunamis approach shallow water, however, the wave amplitude increases.
The wave amplitude is measured by an electro-contact probe.
This wave amplitude is almost undetectable during drilling operations.
The information transported by these waves is encoded in the rapid variation of the wave amplitude.
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Significant differences emerged in slow-wave amplitude (nPAMP) and slope parameters (ADS, MDS, AUS, MUS).
T-wave amplitude was also evaluated as a continuous variable according to infarct location (maximum T-wave amplitude) and as the amount of excess T-wave amplitude above normal (excess T-wave amplitude).
R-wave amplitude and R-wave progression.
Hereafter, we refer to the coda-normalized maximum P-wave amplitude as "P-wave amplitude".
Fig. 5 Maximum S-wave amplitude distribution of each earthquake.
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