Sentence examples for mean horizontal wind from inspiring English sources
Model sensitivity analyses showed that mean horizontal wind velocity, seed release height, and vegetation height are crucial determinants of dispersal potential and dispersal distances.
Figures on the left show total jet occurrence counts (shading) from 6-h ERA-40 fields and the interannual variability of the jet latitude (box plots) from ERA-40 monthly mean horizontal wind.
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.
A meteor radar to measure hourly mean horizontal winds in the 80 100 km height range and daily temperatures near 90 km is operating at Collm (51.3°N, 13°E) since summer 2004.
Daily mean horizontal winds during periods between DOY 120 and 130 obtained by the MF radar observation at Syowa Station are shown in Fig. 5 in order to determine the cause of the enhanced vertical motion.
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.
The inputs used to estimate the sensible heat fluxes included air temperature sampled at 10 Hz, the mean and variance of the horizontal wind speed, the canopy height, and the plant area index for a given intermediate height of the canopy.
The global mean altitude averaged middle atmospheric horizontal wind is 13.2 m/s on the TLE and 27.5 m/s on the PDE.
Thick lines indicate an a 11-year or b 5-year running mean Fig. 6 Monthly averaged horizontal wind at 1000 hPa in May in a 2008 and b 2013.
Fig. 6 The ensemble mean distributions of 1 h rainfall and horizontal wind at the height of 20 m at 12 00 JST, analyzed by the inner LETKF.
A horizontal wind vector field at the cloud-top height will be retrieved by means of a cloud tracking method.
