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Unidirectional signals lasting >25 ms, having intensities of >9 dB were considered to represent embolic events.
Since the change was very slow, it did n ot affect sample normalization and would be noticeable only as weaker-than-expected signals lasting few hours twice a day.
One striking implication of Eq. (10) is that for detection probabilities as large as about 50 60%, for which the number of potentially detectable emitters in the galaxy can reach values well beyond ≈103 even for signals lasting in average 1′000 years (see Fig. 3), the mean number of detectable signals is below one.
Ground-based measurements have captured 10% more deformation signals lasting > 5 years than InSAR, suggesting that the longest duration processes also remain under-represented.
The higher number of InSAR measurements for signal durations of > 12 months (Fig. 4B) reflects the under-representation of signals lasting days to months in our records.
The initial signal was followed by long-duration infrasound signals lasting about 90 minutes after the seismic event; such long wave trains were presumably generated by ground motion around the epicenter and in other regions.
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Both parental genomes undergo large-scale H3K9me3 reestablishment after fertilization, and the imbalance in parental H3K9me3 signals lasts until blastocyst.
The signals lasted 2.5 s and the pause between the signals was random ranging 1.4 5.0 s.
In a characteristic signal lasting one minute, the station identification, in Morse code, is transmitted two or three times, followed by a period of continuous transmission during which a bearing can be taken by a ship's direction-finding receiver.
Approximately 10 h after the arrival of the first seismic wave, we observed a tsunami signal lasting for 5 6 h on the DPG sensor (Fig. 5(c)).
In the LIA mode, the EEG is dominated by sharp waves that are randomly timed large deflections of the EEG signal lasting for 25 50 milliseconds.
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