Sentence examples for mean vertical component from inspiring English sources

Vertical fluctuations were found to decrease though an increase in the mean vertical component.

If we use the same geomagnetic latitude for the four regions, i.e., 45°, where the MSNA and the remnant of the winter anomaly take place, then the mean vertical component of the field-aligned neutral wind (V) values is 20, 41, 31, and 2 m/s for North America, South America, Asia, and Oceania, respectively.

The mean vertical component of velocity of our flies was –0.1 ms.d (s.d. = 0.6 ms−1), indicating that on average they descended a little in flight (Fig. 4C).

The mean bilateral vertical component of the bra breast force in standing was 11.7 ± 4.6 N, whereas during treadmill running the mean unilateral bra breast force was 8.7 ± 6.4 N and 14.7 ± 10.3 N in the high and low support conditions, respectively.

This means that the vertical component of the electric field is determinant for the Esb layer occurrence, in such a way that Esb layer only occurs under low E z values.

The standard deviation of the mean difference values is shown, and the last column is the mean value of the vertical component of the field-aligned neutral wind at 22 LT, using all the data within each region shown in Fig. 2.

This is a 10-min average of the root mean square amplitude of the vertical component seismometer at IJMV, and bandpass filters of 0.1 2 Hz are applied.

The mean values of vTECGNSS, (overline{text{vTEC}}_{{{text{GNSS}} }}), and the mean values of the effective vertical component of the field-aligned neutral wind, (bar{V}_{text{HWM07}}), are computed for the east and west highlighted sectors (Table 3).

It means trying to represent the vertical component of the underlying evolutionary process, i.e. inheritance from parent to offspring.

Residuals of (a) declination (D), (b) horizontal component (H), and (c) vertical component (Z) annual mean values for all days at the six Indian stations, together with annual mean sunspot numbers and the Hale-cycle from 1958 to 2009.

The averaged root mean square (RMS) envelope of the vertical component at each station was calculated by stacking the 15-s envelopes of the normalized seismograms observed for all earthquakes (Figure 4).