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Subsequently, we compare the average number of paths created by each algorithm.
Subsequently, we compare the dispersion patterns, and assess the contribution of each additional process to variability of data.
Subsequently, we compare the coordinates of the stimulation site with the optically-derived coordinates of the excitation origin.
Subsequently, we compare Medicare data with employer-sponsored insurance to explore sensitivity and specificity of these data.
Subsequently, we compare the Nyquist plots for the cell at fixed bias voltage of −0.3 V (close to V oc) and the results are presented in Fig. 13b.
Subsequently, we compare this enhanced, "rational," model to its "non-rational" predecessor and a further control condition using both simulated and real robots, in a variety of environments.
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Subsequently, we compared several voice source parameters including fundamental frequency, jitter, shimmer, harmonicity, and cepstral peak prominence of adult and older males.
Subsequently, we compared the measured data with those of past landscape stages to determine landscape changes and their mechanisms at different spatio-temporal scales.
Subsequently, we compared the estimated turbidite depositional ages with those of onland tsunami deposits reported by previous studies (Sawai et al. 2012; Hirakawa 2012; Takada et al. 2016; Ishimura 2017).
Subsequently, we compared the data obtained for 3-chloro and 2,3-dimethyl derivatives (2 and 4, respectively) and unsubstituted phenylpiperazine analog 1 with those previously reported for their 2,3-dichloro analogs.
Subsequently, we compared the peak ground acceleration (PGA) of the scenario earthquakes generated for this study within the urban tracts for Mérida State to ensure the PGAs used for loss modeling correlate with the 475 and 975 year frequencies of the seismic hazard curve for Mérida State (Fig. 4) from Bendito et al. (2001).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com