Sentence examples for mean vertical wind from inspiring English sources

However, we can see that with a mean vertical wind of 18 m/s, there is a decrease of 8 11% in all regions except for Oceania.

This variability is the result of the combined effect of the neutral composition, mean vertical wind, and the solar irradiation variations.

Here, we compared quantities from eight different model SATs: (i) mean temperature (¯¯¯¯Ts) in an acoustically isolated chamber, (ii) mean vertical wind speed (¯¯¯¯ws) in a low-speed wind tunnel, and (iii) wind statistics with data collected over a research field.

This first mode describes the vTECGNSS variability, caused by the combined effect of the neutral composition, mean vertical wind, the solar irradiation variations (which define the starting conditions before beginning the nighttime loss processes), and the first two modes of V HWM07.

The adjustment times of the TLE total ozone column (({mathrm{TOC}}_{mathrm{TLE}})), the global mean horizontal wind (({mathrm{HW}}_{mathrm{TLE}})), the global mean vertical wind (({mathrm{VW}}_{mathrm{TLE}})) and the global mean stratospheric temperature ((mathrm{T}_{mathrm{strat TLE)}})) to the new tidally locked conditions are shown in Fig. 3.

One explanation is that the mean vertical winds in these two regions during nighttime are two or more times larger than those in North America and Oceania, reaching mean values of 40 m/s during the summer.

Figure 3 shows the adjustment times of the CTLE and WTLE total ozone column (TOC), and the global-mean stratospheric horizontal wind (HW), global-mean stratospheric vertical wind and global-mean stratospheric temperature (T) for the 30 40 km altitude range.

Figure 3a shows AMJ-mean tropospheric thickness and vertical wind shear.

The effects of turbulence intensity, mean wind speed, wind shear, vertical wind component, dynamic stall, stall hysteresis, and blade stiffness were examined.

First, at midnight the behavior of mean vTECGNSS values responds to vertical wind variation, experiencing a decrease of about 10% with the action of the positive vertical wind lasting for 2 h in all regions except Oceania.

At midnight, the behavior of mean vTEC values strongly responds to vertical wind variation, experiencing a decrease of about 10 15% with the action of the positive vertical component of the field-aligned neutral wind lasting for 2 h in all regions except for Oceania.