The PACF is defined as the sequence of correlations between (Y t and Yt−1), (Y t and Yt−2), (Y t and Yt−3), and so on, because the effects of prior lag on t remain constant.
e Temporal sequence of the correlation coefficient between the reference and the microphone seismometer correlation functions during the period from May 21 , 2015 to September 30 , 2016 and f its magnified plot during the eruption Fig. 3 Seismic and microphone records at the OWD station during the rapid tilt change.
An example of a temporal sequence of microphone seismometer correlation functions in the high-frequency range from 02 30 to 06 30 on July 01 , 2015 is indicated in Fig. 2c, d.
The off-peak values are typically Gaussian distributed, as discussed in Section 4, and shown in Fig. 1a. Figure 1b shows the time sequence of the correlations.
Nevertheless, each step we take in the progression of the algorithm increases its performance, and as mentioned in the list above, we have the sequence of rank correlations as 0.535, 0.620, 0.623 and 0.624.
The remarkable conservation of the protein sequences, the unexplained conservation of the intron sequences, the lack of correlation between evolutionary distance and mutation rate, and the pattern of silent vs non-silent codon changes all point to lateral transfer of the gene.
The remarkable conservation of both intron and exon sequences, the lack of correlation between evolutionary distance and mutation rate, and the pattern of silent vs non-silent codon changes make it unlikely that the gene for this AFP pre-existed but was lost from most branches of the teleost radiation.
a RMS amplitude over 1 min for the microphone (red line) and the vertical ground velocity (black line) at the OWD station during the period from 07:00 to 11 00 June 29 , 2015and b a temporal sequence of the microphone seismometer correlation function of the band-passed seismic and infrasonic signals.
c RMS amplitude during the period from 02 30 to 06 30 on July 01 and d a temporal sequence of the cross-correlation function.
While structuring C budgets as a sequence of gain-loss correlations, heterotrophic respiration in soil often represents the end of the sequence, or the final amount of C removed from the terrestrial ecosystem.
